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		<title>Central African Shear Zone - Versionsgeschichte</title>
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		<title>TerriT5899123 am 9. November 2025 um 08:25 Uhr</title>
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		<summary type="html">&lt;p&gt;&lt;/p&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Nächstältere Version&lt;/td&gt;
			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 9. November 2025, 08:25 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;course &lt;/del&gt;from the Gulf of Guinea &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;by means of &lt;/del&gt;Cameroon into Sudan. The construction isn't &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;effectively &lt;/del&gt;understood. The shear zone dates to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;no less than &lt;/del&gt;640 Ma (million years in the past). Motion occurred along the zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/del&gt;the break-up of Gondwanaland &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the Jurassic and Cretaceous durations. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Among &lt;/del&gt;the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;have &lt;/del&gt;been rejuvenated &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;greater &lt;/del&gt;than once before and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the opening of the South Atlantic &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the Cretaceous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;period&lt;/del&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts throughout the Adamawa uplift, a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;submit&lt;/del&gt;-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic activity has occurred along &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;many &lt;/del&gt;of the size of the Cameroon line from 130 Ma to the current, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/del&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt; &amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;this area is thinned in a comparatively &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;slender &lt;/del&gt;belt, with the asthenosphere upwelling from a depth of about 190 km to about a hundred and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://pasarinko.zeroweb.kr/bbs/board.php?bo_table=notice&amp;amp;wr_id=7684451 Wood Ranger Power Shears warranty] [http://jimiantech.com/g5/bbs/board.php?bo_table=w0dace2gxo&amp;amp;wr_id=435632 Wood Ranger Power Shears price] [https://git.zhukovsky.me/latiajardine9 Power Shears] features &lt;/del&gt;twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;previously &lt;/del&gt;thought to increase eastward solely to the Darfur area of western Sudan. It&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/del&gt;now interpreted to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;extend &lt;/del&gt;into central and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; cordless [https://gitlab.zuisishu.com/yvettestaten05 Wood Ranger Power Shears order now] [http://jicc.kr/bbs/board.php?bo_table=hosung3&amp;amp;wr_id=646519 garden power shears] &lt;/del&gt;eastern Sudan, with a total size of 4,000 km. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;In &lt;/del&gt;the Sudan, the shear zone might have acted as a structural barrier to improvement of deep Cretaceous-Tertiary sedimentary basins in the north of the world. Objections to this &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;concept &lt;/del&gt;are that the Bahr el Arab and Blue Nile rifts extend northwest &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;past &lt;/del&gt;one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;on &lt;/del&gt;this areas &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;supports &lt;/del&gt;the theory. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://digitalmarketinghints.xyz/index.php?title=User:AlexisDobbins6 buy Wood Ranger Power Shears] &lt;/del&gt;Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Dorbath, C.; &lt;/del&gt;Dorbath,&amp;#160; [https://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;healthwiz&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;co.uk&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;index.php?title=Bird_Stewart_Lightfoot_2025_P buy &lt;/del&gt;Wood Ranger Power Shears] L.; Fairhead, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://www.vokipedia.de/index.php?title=Benutzer:ShannonCarringto buy Wood Ranger Power Shears] &lt;/del&gt;J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time study &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/del&gt;the Central African Shear Zone within the Adamawa &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;region &lt;/del&gt;of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/del&gt;research&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/del&gt;the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://leadwith.org/bbs/board.php?bo_table=free&amp;amp;wr_id=383581 buy Wood Ranger Power Shears] &lt;/del&gt;L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure throughout the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;One &lt;/del&gt;hundred fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics, financial geology, geohazards, geosites and geoscientific education of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;each nation&lt;/del&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;charge&lt;/del&gt;-dependent resistance to a change in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shape &lt;/del&gt;or to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement &lt;/del&gt;of its neighboring parts relative to each other. For liquids, it corresponds to the informal idea of thickness; for &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;example&lt;/del&gt;, syrup has a better viscosity than water. Viscosity is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;defined &lt;/del&gt;scientifically as a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;drive &lt;/del&gt;multiplied by a time divided by an space. Thus its SI &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;models &lt;/del&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;internal &lt;/del&gt;frictional &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/del&gt;between adjoining layers of fluid which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/del&gt;in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;For &lt;/del&gt;example, when a viscous fluid is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;forced &lt;/del&gt;by a tube, it flows extra &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;rapidly &lt;/del&gt;near the tube's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;center &lt;/del&gt;line than close to its walls. Experiments &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;show &lt;/del&gt;that some stress (similar to a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;stress &lt;/del&gt;distinction between the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;two &lt;/del&gt;ends of the tube) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;needed &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;maintain &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;move&lt;/del&gt;. It &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/del&gt;because a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://git.van-peeren.de/norrisdenton71 buy Wood Ranger Power Shears] &lt;/del&gt;is required to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;overcome &lt;/del&gt;the friction between the layers of the fluid &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;that &lt;/del&gt;are in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/del&gt;. For a tube with a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constant price &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;energy &lt;/del&gt;of the compensating &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/del&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Generally&lt;/del&gt;, viscosity depends upon a fluid's state, similar to its temperature, pressure, and price of deformation. However, the dependence on a few of these properties is negligible in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sure cases&lt;/del&gt;. For &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;example&lt;/del&gt;, the viscosity of a Newtonian fluid doesn't &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;vary considerably &lt;/del&gt;with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;speed &lt;/del&gt;of deformation. Zero viscosity (no resistance to shear stress) is observed solely at very low temperatures in superfluids; otherwise, the second law of thermodynamics requires all fluids to have &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructive &lt;/del&gt;viscosity. A fluid that has zero viscosity (non-viscous) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;called very best &lt;/del&gt;or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which can be &lt;/del&gt;time-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;independent&lt;/del&gt;, and there are thixotropic and rheopectic flows &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which &lt;/del&gt;are time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;additionally &lt;/del&gt;referred to a viscous glue derived from mistletoe berries. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;materials &lt;/del&gt;science and engineering, there is often curiosity in understanding the forces or stresses concerned within the deformation of a material.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;path &lt;/ins&gt;from the Gulf of Guinea &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/ins&gt;Cameroon into Sudan. The construction &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;just &lt;/ins&gt;isn't &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;nicely &lt;/ins&gt;understood. The shear zone dates to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;at least &lt;/ins&gt;640 Ma (million years in the past). Motion occurred along the zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;during &lt;/ins&gt;the break-up of Gondwanaland &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the Jurassic and Cretaceous durations. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;A few of &lt;/ins&gt;the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;had &lt;/ins&gt;been rejuvenated &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;more &lt;/ins&gt;than once before and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in the course of &lt;/ins&gt;the opening of the South Atlantic &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the Cretaceous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;interval&lt;/ins&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts throughout the Adamawa uplift, a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;put up&lt;/ins&gt;-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic activity has occurred along &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a lot &lt;/ins&gt;of the size of the Cameroon line from 130 Ma to the current, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;could also &lt;/ins&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;on &lt;/ins&gt;this area is thinned in a comparatively &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;narrow &lt;/ins&gt;belt, with the asthenosphere upwelling from a depth of about 190 km to about a hundred and twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;formerly &lt;/ins&gt;thought to increase eastward solely to the Darfur area of western Sudan. It &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/ins&gt;now interpreted to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;increase &lt;/ins&gt;into central and eastern Sudan, with a total size of 4,000 km. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Within &lt;/ins&gt;the Sudan, the shear zone might have acted as a structural barrier to improvement of deep Cretaceous-Tertiary sedimentary basins in the north of the world. Objections to this &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;idea &lt;/ins&gt;are that the Bahr el Arab and Blue Nile rifts extend northwest &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;beyond &lt;/ins&gt;one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;this areas &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;helps &lt;/ins&gt;the theory. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://swagatamtraditions.com/how-one-can-thin-your-personal-hair-with-thinning-shears/ Wood Ranger Power Shears shop] &lt;/ins&gt;pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://8.138.4.170:8980/vernapipkin51 Wood Ranger Power Shears for sale] [https://www.office-ems.jp/cropped-ems_favicon-5-gif/ Wood Ranger Power Shears shop] [https://git.fram.i.ng/kaleygjd696179 Wood Ranger Power Shears specs] Shears features &lt;/ins&gt;pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath,&amp;#160; [https://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;agnantihotel&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;gr/faq-items/integer-vitae-nisl-non-augue-ullamcorper-blandit-donec-vitae-nibh-ipsums&lt;/ins&gt;/ Wood Ranger Power Shears &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shop&lt;/ins&gt;] &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;C.; Dorbath, &lt;/ins&gt;L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time study &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the Central African Shear Zone within the Adamawa &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/ins&gt;of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;subject &lt;/ins&gt;research&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure throughout the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;A &lt;/ins&gt;hundred &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;and &lt;/ins&gt;fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics, financial geology, geohazards, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://srv482333.hstgr.cloud/index.php/24-Month_Inshearance®_Warranty Wood Ranger Power Shears shop] &lt;/ins&gt;geosites and geoscientific education of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;every country&lt;/ins&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rate&lt;/ins&gt;-dependent resistance to a change in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;form &lt;/ins&gt;or to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion &lt;/ins&gt;of its neighboring parts relative to each other. For liquids, it corresponds to the informal idea of thickness; for &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;instance&lt;/ins&gt;, syrup has a better viscosity than water. Viscosity is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;outlined &lt;/ins&gt;scientifically as a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/ins&gt;multiplied by a time divided by an space. Thus its SI &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;units &lt;/ins&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;interior&amp;#160; [https://lunarishollows.wiki/index.php?title=This_Adaptation_Incorporates_The_Rotation_Circuit Wood Ranger Power Shears shop] &lt;/ins&gt;frictional &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;drive &lt;/ins&gt;between adjoining layers of fluid which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;might be &lt;/ins&gt;in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;As an &lt;/ins&gt;example, when a viscous fluid is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;compelled &lt;/ins&gt;by &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;way of &lt;/ins&gt;a tube, it flows extra &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shortly &lt;/ins&gt;near the tube's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;middle &lt;/ins&gt;line than close to its walls. Experiments &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;present &lt;/ins&gt;that some stress (similar to a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/ins&gt;distinction between the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;2 &lt;/ins&gt;ends of the tube) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;required &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sustain &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;circulation&lt;/ins&gt;. It&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/ins&gt;because a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;power &lt;/ins&gt;is required to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;beat &lt;/ins&gt;the friction between the layers of the fluid &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;which &lt;/ins&gt;are in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;. For &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://king-wifi.win/wiki/Varieties_Of_Pruning_Shears buy Wood Ranger Power Shears] &lt;/ins&gt;a tube with a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;continuing rate &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;circulate&lt;/ins&gt;, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[https://higgledy-piggledy.xyz/index.php/The_Best_Pruning_Shears_For_2025 electric power shears] &lt;/ins&gt;of the compensating &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[http://www.infinitymugenteam.com:80/infinity.wiki/mediawiki2/index.php/User:LorenDooley86 Wood Ranger Power Shears shop] &lt;/ins&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Typically&lt;/ins&gt;, viscosity depends upon a fluid's state, similar to its temperature, pressure, and price of deformation. However, the dependence on a few of these properties is negligible in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;certain circumstances&lt;/ins&gt;. For &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://wiki.dulovic.tech/index.php/User:LanoraRaine594 Wood Ranger Power Shears shop] instance&lt;/ins&gt;, the viscosity of a Newtonian fluid doesn't &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;fluctuate significantly &lt;/ins&gt;with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rate &lt;/ins&gt;of deformation. Zero viscosity (no resistance to shear stress) is observed solely at very low temperatures in superfluids; otherwise, the second law of thermodynamics requires all fluids to have &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;positive &lt;/ins&gt;viscosity. A fluid that has zero viscosity (non-viscous) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as preferrred &lt;/ins&gt;or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;that are &lt;/ins&gt;time-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;unbiased&lt;/ins&gt;, and there are thixotropic and rheopectic flows &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;that &lt;/ins&gt;are time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;also &lt;/ins&gt;referred to a viscous glue derived from mistletoe berries. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;supplies &lt;/ins&gt;science and engineering, there is often curiosity in understanding the forces or stresses concerned within the deformation of a material.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>TerriT5899123</name></author>	</entry>

	<entry>
		<id>http://www.vokipedia.de/index.php?title=Central_African_Shear_Zone&amp;diff=208969&amp;oldid=prev</id>
		<title>TLTRod1067 am 31. Oktober 2025 um 13:43 Uhr</title>
		<link rel="alternate" type="text/html" href="http://www.vokipedia.de/index.php?title=Central_African_Shear_Zone&amp;diff=208969&amp;oldid=prev"/>
				<updated>2025-10-31T13:43:50Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class='diff diff-contentalign-left'&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 31. Oktober 2025, 13:43 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;path &lt;/del&gt;from the Gulf of Guinea by means of Cameroon into Sudan. The construction &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is just not nicely &lt;/del&gt;understood. The shear zone dates to no less than 640 Ma (million years &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;ago&lt;/del&gt;). Motion occurred along the zone through the break-up of Gondwanaland &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the Jurassic and Cretaceous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;periods&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Some of &lt;/del&gt;the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;had &lt;/del&gt;been rejuvenated greater than once before and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/del&gt;the opening of the South Atlantic &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the Cretaceous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;interval&lt;/del&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts throughout the Adamawa uplift, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://wiki.dulovic.tech/index.php/THE_HAIR_STYLIST%E2%80%99S_Choice Wood Ranger Power Shears website] &lt;/del&gt;a submit-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic activity has occurred &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;alongside &lt;/del&gt;many of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;length &lt;/del&gt;of the Cameroon line from 130 Ma to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;present&lt;/del&gt;, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;could also &lt;/del&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;on &lt;/del&gt;this area is thinned in a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;relatively &lt;/del&gt;slender belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;one &lt;/del&gt;hundred twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;formerly &lt;/del&gt;thought to increase eastward &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;only &lt;/del&gt;to the Darfur &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;region &lt;/del&gt;of western Sudan. It &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/del&gt;now interpreted to extend into central and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;jap &lt;/del&gt;Sudan, with a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;complete &lt;/del&gt;size of 4,000 km. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Within &lt;/del&gt;the Sudan, the shear zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/del&gt;have acted as a structural barrier to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;growth &lt;/del&gt;of deep Cretaceous-Tertiary sedimentary basins in the north of the world. Objections to this concept are that the Bahr el Arab and Blue Nile rifts extend northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;this areas &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;helps &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;idea&lt;/del&gt;. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;research &lt;/del&gt;across the Central African Shear Zone within the Adamawa &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/del&gt;of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential area &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;studies&lt;/del&gt;&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations across the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;construction across &lt;/del&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;A &lt;/del&gt;hundred &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;and &lt;/del&gt;fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;economic &lt;/del&gt;geology, geohazards, geosites and geoscientific &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;training &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;every country&lt;/del&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;rate&lt;/del&gt;-dependent resistance to a change in shape or to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion &lt;/del&gt;of its neighboring &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;portions &lt;/del&gt;relative to each other. For liquids, it corresponds to the informal idea of thickness; for example, syrup has a better viscosity than water. Viscosity is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;outlined &lt;/del&gt;scientifically as a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/del&gt;multiplied by a time divided by an &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;area&lt;/del&gt;. Thus its SI models are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;inner &lt;/del&gt;frictional &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://git.dadunode.com/dorrisminter20 Wood Ranger Power Shears website] &lt;/del&gt;between &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;adjacent &lt;/del&gt;layers of fluid which are in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/del&gt;. For example, when a viscous fluid is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;compelled &lt;/del&gt;by &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;way of &lt;/del&gt;a tube, it flows extra rapidly &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;close to &lt;/del&gt;the tube's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;heart &lt;/del&gt;line than &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;near &lt;/del&gt;its &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;partitions&lt;/del&gt;. Experiments &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;present &lt;/del&gt;that some stress (&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;resembling &lt;/del&gt;a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/del&gt;distinction between the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;2 &lt;/del&gt;ends of the tube) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;required &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sustain &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;This &lt;/del&gt;is because a [&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;http&lt;/del&gt;://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;repo&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;fusi24&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;com:3000&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;kaibarron6430 &lt;/del&gt;Wood Ranger Power Shears &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;for sale&lt;/del&gt;] is required to overcome the friction between the layers of the fluid &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which &lt;/del&gt;are in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;. For a tube with a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;relentless rate &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;circulation&lt;/del&gt;, the energy of the compensating &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/del&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Generally, viscosity &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;will depend on &lt;/del&gt;a fluid's state, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;reminiscent of &lt;/del&gt;its temperature, pressure, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;rate &lt;/del&gt;of deformation. However, the dependence on &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;some &lt;/del&gt;of these properties is negligible in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;certain instances&lt;/del&gt;. For example, the viscosity of a Newtonian fluid doesn't &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;range significantly &lt;/del&gt;with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;rate &lt;/del&gt;of deformation. Zero viscosity (no resistance to shear stress) is observed solely at very low temperatures in superfluids; otherwise, the second law of thermodynamics requires all fluids to have &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;positive &lt;/del&gt;viscosity. A fluid that has zero viscosity (non-viscous) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;named ultimate &lt;/del&gt;or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows which can be time-independent, and there are thixotropic and rheopectic flows which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;can be &lt;/del&gt;time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum additionally referred to a viscous glue derived from mistletoe berries. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;supplies &lt;/del&gt;science and engineering, there is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;usually &lt;/del&gt;curiosity in understanding the forces or stresses &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;involved in &lt;/del&gt;the deformation of a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;fabric&lt;/del&gt;.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;course &lt;/ins&gt;from the Gulf of Guinea by means of Cameroon into Sudan. The construction &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;isn't effectively &lt;/ins&gt;understood. The shear zone dates to no less than 640 Ma (million years &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in the past&lt;/ins&gt;). Motion occurred along the zone through the break-up of Gondwanaland &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the Jurassic and Cretaceous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;durations&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Among &lt;/ins&gt;the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;have &lt;/ins&gt;been rejuvenated greater than once before and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the opening of the South Atlantic &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the Cretaceous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;period&lt;/ins&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts throughout the Adamawa uplift, a submit-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic activity has occurred &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;along &lt;/ins&gt;many of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;size &lt;/ins&gt;of the Cameroon line from 130 Ma to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;current&lt;/ins&gt;, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/ins&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt; &amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;this area is thinned in a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;comparatively &lt;/ins&gt;slender belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a &lt;/ins&gt;hundred &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;and&amp;#160; [http://pasarinko.zeroweb.kr/bbs/board.php?bo_table=notice&amp;amp;wr_id=7684451 Wood Ranger Power Shears warranty] [http://jimiantech.com/g5/bbs/board.php?bo_table=w0dace2gxo&amp;amp;wr_id=435632 Wood Ranger Power Shears price] [https://git.zhukovsky.me/latiajardine9 Power Shears] features &lt;/ins&gt;twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;previously &lt;/ins&gt;thought to increase eastward &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;solely &lt;/ins&gt;to the Darfur &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/ins&gt;of western Sudan. It&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/ins&gt;now interpreted to extend into central and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; cordless [https://gitlab.zuisishu.com/yvettestaten05 Wood Ranger Power Shears order now] [http://jicc.kr/bbs/board.php?bo_table=hosung3&amp;amp;wr_id=646519 garden power shears] eastern &lt;/ins&gt;Sudan, with a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;total &lt;/ins&gt;size of 4,000 km. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;In &lt;/ins&gt;the Sudan, the shear zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;might &lt;/ins&gt;have acted as a structural barrier to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;improvement &lt;/ins&gt;of deep Cretaceous-Tertiary sedimentary basins in the north of the world. Objections to this concept are that the Bahr el Arab and Blue Nile rifts extend northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;on &lt;/ins&gt;this areas &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;supports &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;theory&lt;/ins&gt;. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://digitalmarketinghints.xyz/index.php?title=User:AlexisDobbins6 buy Wood Ranger Power Shears] &lt;/ins&gt;Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://healthwiz.co.uk/index.php?title=Bird_Stewart_Lightfoot_2025_P buy Wood Ranger Power Shears] &lt;/ins&gt;L.; Fairhead, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://www.vokipedia.de/index.php?title=Benutzer:ShannonCarringto buy Wood Ranger Power Shears] &lt;/ins&gt;J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;study &lt;/ins&gt;across the Central African Shear Zone within the Adamawa &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;region &lt;/ins&gt;of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential area &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;research&lt;/ins&gt;&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations across the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://leadwith.org/bbs/board.php?bo_table=free&amp;amp;wr_id=383581 buy Wood Ranger Power Shears] &lt;/ins&gt;L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;structure throughout &lt;/ins&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;One &lt;/ins&gt;hundred fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;financial &lt;/ins&gt;geology, geohazards, geosites and geoscientific &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;education &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;each nation&lt;/ins&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;charge&lt;/ins&gt;-dependent resistance to a change in shape or to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement &lt;/ins&gt;of its neighboring &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;parts &lt;/ins&gt;relative to each other. For liquids, it corresponds to the informal idea of thickness; for example, syrup has a better viscosity than water. Viscosity is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;defined &lt;/ins&gt;scientifically as a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;drive &lt;/ins&gt;multiplied by a time divided by an &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;space&lt;/ins&gt;. Thus its SI models are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;internal &lt;/ins&gt;frictional &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/ins&gt;between &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;adjoining &lt;/ins&gt;layers of fluid which are in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;. For example, when a viscous fluid is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;forced &lt;/ins&gt;by a tube, it flows extra rapidly &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;near &lt;/ins&gt;the tube's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;center &lt;/ins&gt;line than &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;close to &lt;/ins&gt;its &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;walls&lt;/ins&gt;. Experiments &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;show &lt;/ins&gt;that some stress (&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;similar to &lt;/ins&gt;a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;stress &lt;/ins&gt;distinction between the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;two &lt;/ins&gt;ends of the tube) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;needed &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;maintain &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;move&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;It &lt;/ins&gt;is because a [&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;https&lt;/ins&gt;://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;git&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;van-peeren&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;de&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;norrisdenton71 buy &lt;/ins&gt;Wood Ranger Power Shears] is required to overcome the friction between the layers of the fluid &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;that &lt;/ins&gt;are in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/ins&gt;. For a tube with a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constant price &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;, the energy of the compensating &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/ins&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Generally, viscosity &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;depends upon &lt;/ins&gt;a fluid's state, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;similar to &lt;/ins&gt;its temperature, pressure, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;price &lt;/ins&gt;of deformation. However, the dependence on &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a few &lt;/ins&gt;of these properties is negligible in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sure cases&lt;/ins&gt;. For example, the viscosity of a Newtonian fluid doesn't &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;vary considerably &lt;/ins&gt;with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;speed &lt;/ins&gt;of deformation. Zero viscosity (no resistance to shear stress) is observed solely at very low temperatures in superfluids; otherwise, the second law of thermodynamics requires all fluids to have &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constructive &lt;/ins&gt;viscosity. A fluid that has zero viscosity (non-viscous) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;called very best &lt;/ins&gt;or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows which can be time-independent, and there are thixotropic and rheopectic flows which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/ins&gt;time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum additionally referred to a viscous glue derived from mistletoe berries. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;materials &lt;/ins&gt;science and engineering, there is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;often &lt;/ins&gt;curiosity in understanding the forces or stresses &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;concerned within &lt;/ins&gt;the deformation of a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;material&lt;/ins&gt;.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>TLTRod1067</name></author>	</entry>

	<entry>
		<id>http://www.vokipedia.de/index.php?title=Central_African_Shear_Zone&amp;diff=135792&amp;oldid=prev</id>
		<title>DarrenEsmond32 am 15. September 2025 um 10:42 Uhr</title>
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				<updated>2025-09-15T10:42:35Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 15. September 2025, 10:42 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;direction &lt;/del&gt;from the Gulf of Guinea &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;via &lt;/del&gt;Cameroon into Sudan. The construction is not &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;well &lt;/del&gt;understood. The shear zone dates to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a minimum of &lt;/del&gt;640 Ma (million years &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in the past&lt;/del&gt;). Motion occurred &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;alongside &lt;/del&gt;the zone through the break-up of Gondwanaland &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://www.wakewiki.de/index.php?title=How_You_Can_Sharpen_Kitchen_Shears_5_Easy_Methods professional landscaping shears] &lt;/del&gt;within the Jurassic and Cretaceous periods. Some of the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;were &lt;/del&gt;rejuvenated &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;more than as soon as earlier &lt;/del&gt;than and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in the course of &lt;/del&gt;the opening of the South Atlantic &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the Cretaceous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;period&lt;/del&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts throughout the Adamawa uplift, a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;put up&lt;/del&gt;-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;exercise &lt;/del&gt;has occurred alongside &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a lot &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;size &lt;/del&gt;of the Cameroon line from 130 Ma to the present, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/del&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ on this area is thinned in a relatively &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;slim &lt;/del&gt;belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a &lt;/del&gt;hundred &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;and &lt;/del&gt;twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was formerly thought to increase eastward only to the Darfur region of western Sudan. It&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/del&gt;now interpreted to extend into central and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;japanese &lt;/del&gt;Sudan, with a complete &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;length &lt;/del&gt;of 4,000 km. Within the Sudan, the shear zone may have acted as a structural barrier to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;improvement &lt;/del&gt;of deep Cretaceous-Tertiary sedimentary basins &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the north of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;realm&lt;/del&gt;. Objections to this &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;idea &lt;/del&gt;are that the Bahr el Arab and Blue Nile rifts extend northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts in this areas helps the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;theory&lt;/del&gt;. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://lunarishollows.wiki/index.php?title=User:MarcMoller0813 professional landscaping shears] &lt;/del&gt;pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;study &lt;/del&gt;across the Central African Shear Zone within the Adamawa area of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://rentry.co/29348-when-you-suspect-a-freon-problem Wood Ranger Power Shears website] [https://brogue.wiki/mw/index.php?title=Our_Picks_For_The_Very_Best_Pruning_Shears_For_Gardening_For_2025 Wood Ranger Power Shears price] Power Shears manual &lt;/del&gt;planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;discipline &lt;/del&gt;studies&amp;quot;. Pankhurst, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://gummipuppen-wiki.de/index.php?title=Benutzer:JuliusPak557552 Wood Ranger Power Shears USA] [https://dev.neos.epss.ucla.edu/wiki/index.php?title=Why_It_s_Best_To_Personal_A_Pair_Of_Fine_Kitchen_Shears Wood Ranger Power Shears manual] [https://wiki.dulovic.tech/index.php/Since_We_Use_Non-linear_Artificial_Diffusion garden power shears] Shears &lt;/del&gt;Robert J. (2008). West Gondwana: pre-Cenozoic correlations across the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;structure throughout &lt;/del&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. A hundred and fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://rentry.co/50226-answers-about-flower-gardening professional landscaping shears] &lt;/del&gt;Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;financial &lt;/del&gt;geology, geohazards, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://healthwiz.co.uk/index.php?title=Now_Alligator_Shears_Are_Hydraulically_Actuated professional landscaping shears] &lt;/del&gt;geosites and geoscientific &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;education &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;each nation&lt;/del&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;charge&lt;/del&gt;-dependent resistance to a change in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;form &lt;/del&gt;or to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement &lt;/del&gt;of its neighboring &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;parts &lt;/del&gt;relative to each other. For liquids, it corresponds to the informal &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;concept &lt;/del&gt;of thickness; for &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;instance&lt;/del&gt;, syrup has a better viscosity than water. Viscosity is outlined scientifically as a force multiplied by a time divided by an area. Thus its SI &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;items &lt;/del&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;internal &lt;/del&gt;frictional &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;power &lt;/del&gt;between &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;adjoining &lt;/del&gt;layers of fluid which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;might be &lt;/del&gt;in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;As an illustration&lt;/del&gt;, when a viscous fluid is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressured through &lt;/del&gt;a tube, it flows extra &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shortly &lt;/del&gt;close to the tube's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;center &lt;/del&gt;line than near its partitions. Experiments present that some stress (&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;similar to &lt;/del&gt;a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;stress &lt;/del&gt;distinction between the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;two &lt;/del&gt;ends of the tube) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;needed &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;maintain &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;circulate&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;It &lt;/del&gt;is because a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;power &lt;/del&gt;is required to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;beat &lt;/del&gt;the friction between the layers of the fluid which are in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/del&gt;. For a tube with a relentless rate of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;power &lt;/del&gt;of the compensating &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;drive &lt;/del&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;In general&lt;/del&gt;, viscosity &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;depends &lt;/del&gt;on a fluid's state, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;akin to &lt;/del&gt;its temperature, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;stress&lt;/del&gt;, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;price &lt;/del&gt;of deformation. However, the dependence on &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a few &lt;/del&gt;of these properties is negligible in certain &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cases&lt;/del&gt;. For &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;instance&lt;/del&gt;, the viscosity of a Newtonian fluid doesn't &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;vary considerably &lt;/del&gt;with the rate of deformation. Zero viscosity (no resistance to shear stress) is observed solely at very low temperatures in superfluids; &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in any other case&lt;/del&gt;, the second &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;regulation &lt;/del&gt;of thermodynamics requires all fluids to have positive viscosity. A fluid that has zero viscosity (non-viscous) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;called splendid &lt;/del&gt;or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://43.136.48.165:3003/rhystravis1111/7732961/wiki/Following+the+Skirting+of+the+Fleece professional landscaping shears] &lt;/del&gt;inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/del&gt;time-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;unbiased&lt;/del&gt;, and there are thixotropic and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://www.wakewiki.de/index.php?title=Benutzer:DamienCarls0 professional landscaping shears] &lt;/del&gt;rheopectic flows which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;might &lt;/del&gt;be time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;also &lt;/del&gt;referred to a viscous glue derived from mistletoe berries. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;materials &lt;/del&gt;science and engineering, there is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;commonly interest &lt;/del&gt;in understanding the forces or stresses involved in the deformation of a fabric.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;path &lt;/ins&gt;from the Gulf of Guinea &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;by means of &lt;/ins&gt;Cameroon into Sudan. The construction is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;just &lt;/ins&gt;not &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;nicely &lt;/ins&gt;understood. The shear zone dates to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;no less than &lt;/ins&gt;640 Ma (million years &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;ago&lt;/ins&gt;). Motion occurred &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;along &lt;/ins&gt;the zone through the break-up of Gondwanaland within the Jurassic and Cretaceous periods. Some of the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;had been &lt;/ins&gt;rejuvenated &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;greater &lt;/ins&gt;than &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;once before &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/ins&gt;the opening of the South Atlantic &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the Cretaceous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;interval&lt;/ins&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts throughout the Adamawa uplift, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://wiki.dulovic.tech/index.php/THE_HAIR_STYLIST%E2%80%99S_Choice Wood Ranger Power Shears website] &lt;/ins&gt;a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;submit&lt;/ins&gt;-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;activity &lt;/ins&gt;has occurred alongside &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;many &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;length &lt;/ins&gt;of the Cameroon line from 130 Ma to the present, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;could also &lt;/ins&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ on this area is thinned in a relatively &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;slender &lt;/ins&gt;belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;one &lt;/ins&gt;hundred twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was formerly thought to increase eastward only to the Darfur region of western Sudan. It &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/ins&gt;now interpreted to extend into central and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;jap &lt;/ins&gt;Sudan, with a complete &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;size &lt;/ins&gt;of 4,000 km. Within the Sudan, the shear zone may have acted as a structural barrier to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;growth &lt;/ins&gt;of deep Cretaceous-Tertiary sedimentary basins &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the north of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;world&lt;/ins&gt;. Objections to this &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;concept &lt;/ins&gt;are that the Bahr el Arab and Blue Nile rifts extend northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts in this areas helps the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;idea&lt;/ins&gt;. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;research &lt;/ins&gt;across the Central African Shear Zone within the Adamawa area of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/ins&gt;studies&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations across the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;construction across &lt;/ins&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. A hundred and fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;economic &lt;/ins&gt;geology, geohazards, geosites and geoscientific &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;training &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;every country&lt;/ins&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rate&lt;/ins&gt;-dependent resistance to a change in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shape &lt;/ins&gt;or to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion &lt;/ins&gt;of its neighboring &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;portions &lt;/ins&gt;relative to each other. For liquids, it corresponds to the informal &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;idea &lt;/ins&gt;of thickness; for &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;example&lt;/ins&gt;, syrup has a better viscosity than water. Viscosity is outlined scientifically as a force multiplied by a time divided by an area. Thus its SI &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;models &lt;/ins&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;inner &lt;/ins&gt;frictional &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[https://git.dadunode.com/dorrisminter20 Wood Ranger Power Shears website] &lt;/ins&gt;between &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;adjacent &lt;/ins&gt;layers of fluid which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/ins&gt;in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;For example&lt;/ins&gt;, when a viscous fluid is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;compelled by way of &lt;/ins&gt;a tube, it flows extra &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rapidly &lt;/ins&gt;close to the tube's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;heart &lt;/ins&gt;line than near its partitions. Experiments present that some stress (&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;resembling &lt;/ins&gt;a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/ins&gt;distinction between the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;2 &lt;/ins&gt;ends of the tube) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;required &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sustain &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;This &lt;/ins&gt;is because a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[http://repo.fusi24.com:3000/kaibarron6430 Wood Ranger Power Shears for sale] &lt;/ins&gt;is required to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;overcome &lt;/ins&gt;the friction between the layers of the fluid which are in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;. For a tube with a relentless rate of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;circulation&lt;/ins&gt;, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;energy &lt;/ins&gt;of the compensating &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/ins&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Generally&lt;/ins&gt;, viscosity &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;will depend &lt;/ins&gt;on a fluid's state, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;reminiscent of &lt;/ins&gt;its temperature, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;pressure&lt;/ins&gt;, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rate &lt;/ins&gt;of deformation. However, the dependence on &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;some &lt;/ins&gt;of these properties is negligible in certain &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;instances&lt;/ins&gt;. For &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;example&lt;/ins&gt;, the viscosity of a Newtonian fluid doesn't &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;range significantly &lt;/ins&gt;with the rate of deformation. Zero viscosity (no resistance to shear stress) is observed solely at very low temperatures in superfluids; &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;otherwise&lt;/ins&gt;, the second &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;law &lt;/ins&gt;of thermodynamics requires all fluids to have positive viscosity. A fluid that has zero viscosity (non-viscous) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;named ultimate &lt;/ins&gt;or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;can be &lt;/ins&gt;time-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;independent&lt;/ins&gt;, and there are thixotropic and rheopectic flows which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;can &lt;/ins&gt;be time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;additionally &lt;/ins&gt;referred to a viscous glue derived from mistletoe berries. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;supplies &lt;/ins&gt;science and engineering, there is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;usually curiosity &lt;/ins&gt;in understanding the forces or stresses involved in the deformation of a fabric.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>DarrenEsmond32</name></author>	</entry>

	<entry>
		<id>http://www.vokipedia.de/index.php?title=Central_African_Shear_Zone&amp;diff=117274&amp;oldid=prev</id>
		<title>ShaynaCross am 2. September 2025 um 11:13 Uhr</title>
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				<updated>2025-09-02T11:13:33Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 2. September 2025, 11:13 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
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&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;by means of &lt;/del&gt;Cameroon into Sudan. The &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;structure just isn't &lt;/del&gt;well understood. The shear zone dates to a minimum of 640 Ma (million years in the past). Motion occurred alongside the zone through the break-up of Gondwanaland &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the Jurassic and Cretaceous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;intervals&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;A few &lt;/del&gt;of the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;had been &lt;/del&gt;rejuvenated more than &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;once &lt;/del&gt;earlier than and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/del&gt;the opening of the South Atlantic in the Cretaceous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;interval&lt;/del&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/del&gt;the Adamawa uplift, a put up-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic exercise has occurred alongside &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;most &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;length &lt;/del&gt;of the Cameroon line from 130 Ma to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;current&lt;/del&gt;, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;could also &lt;/del&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ on this &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;space &lt;/del&gt;is thinned in a relatively slim belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;one &lt;/del&gt;hundred twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;previously &lt;/del&gt;thought to increase eastward &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;solely &lt;/del&gt;to the Darfur &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/del&gt;of western Sudan. It &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/del&gt;now interpreted to extend into central and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;eastern &lt;/del&gt;Sudan, with a complete &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;size &lt;/del&gt;of 4,000 km. Within the Sudan, the shear zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;could &lt;/del&gt;have acted as a structural barrier to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;development &lt;/del&gt;of deep Cretaceous-Tertiary sedimentary basins &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the north of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;area&lt;/del&gt;. Objections to this idea are that the Bahr el Arab and Blue Nile rifts extend northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;on &lt;/del&gt;this areas helps the theory. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://wiki.monnaie-libre.fr/wiki/From_2025_By_2025 outdoor trimming tool] &lt;/del&gt;G. W. (1986). &amp;quot;A teleseismic delay time study across the Central African Shear Zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the Adamawa area of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;subject research&lt;/del&gt;&amp;quot;. Pankhurst, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Robert J&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;(2008)&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;West Gondwana&lt;/del&gt;: &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; &lt;/del&gt;[https://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;aeshma&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;net&lt;/del&gt;/index.php/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Quality_Used_Machinery outdoor trimming tool&lt;/del&gt;] pre-Cenozoic correlations &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/del&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;115 &lt;/del&gt;(2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy,&amp;#160; [&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;http&lt;/del&gt;://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;wiki&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;wild-sau&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;com&lt;/del&gt;/index.php?title=&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Thinning_Shears_Vs_Texturizing_Shears_-_Ask_A_Hairstylist outdoor trimming tool&lt;/del&gt;] &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;tectonics, economic geology, geohazards, &lt;/del&gt;geosites and geoscientific &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;schooling &lt;/del&gt;of each nation. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt; &amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's charge-dependent resistance to a change in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shape &lt;/del&gt;or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://bbarlock.com/index.php/Expert_Collection_Man_Box outdoor trimming tool] &lt;/del&gt;to movement of its neighboring &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;portions &lt;/del&gt;relative to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;one another&lt;/del&gt;. For liquids, it corresponds to the informal concept of thickness; for &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;example&lt;/del&gt;, syrup has &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the next &lt;/del&gt;viscosity than water. Viscosity is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;defined &lt;/del&gt;scientifically as a force multiplied by a time divided by an area. Thus its SI &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;units &lt;/del&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the internal frictional &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://koreanaggies.net/board_Lmao72/1920402 Wood Ranger Power Shears for sale] &lt;/del&gt;between &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;adjacent &lt;/del&gt;layers of fluid which might be in relative movement. As an illustration, when a viscous fluid is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;forced by way of &lt;/del&gt;a tube, it flows extra &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;quickly &lt;/del&gt;close to the tube's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;middle &lt;/del&gt;line than near its partitions. Experiments present that some stress (&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;corresponding &lt;/del&gt;to a stress distinction between the two ends of the tube) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;required &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sustain &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;stream&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;This &lt;/del&gt;is because a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/del&gt;is required to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;overcome &lt;/del&gt;the friction between the layers of the fluid &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;that &lt;/del&gt;are in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;. For a tube with a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constant fee &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;circulation&lt;/del&gt;, the power of the compensating &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/del&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;In general, viscosity depends on a fluid's state, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;comparable &lt;/del&gt;to its temperature, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressure&lt;/del&gt;, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;fee &lt;/del&gt;of deformation. However, the dependence on a few of these properties is negligible in certain &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;circumstances&lt;/del&gt;. For instance, the viscosity of a Newtonian fluid doesn't &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;fluctuate &lt;/del&gt;considerably with the rate of deformation. Zero viscosity (no resistance to shear stress) is observed &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;only &lt;/del&gt;at very low temperatures in superfluids; in any other case, the second regulation of thermodynamics requires all fluids to have &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructive &lt;/del&gt;viscosity. A fluid that has zero viscosity (non-viscous) &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as ideally suited &lt;/del&gt;or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;inviscid. For non-Newtonian fluids' viscosity, &lt;/del&gt; [&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;https&lt;/del&gt;://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pipewiki&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;org&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;wiki&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;index.php&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;User:YukikoCorbitt8 outdoor trimming tool&lt;/del&gt;] there are pseudoplastic, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://git.sparrowcomm.com/bradberg554612 outdoor trimming tool] &lt;/del&gt;plastic, and dilatant flows which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;might be &lt;/del&gt;time-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;independent&lt;/del&gt;, and there are thixotropic and rheopectic flows &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;that are &lt;/del&gt;time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum also referred to a viscous glue derived from mistletoe berries. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;supplies &lt;/del&gt;science and engineering, there is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;usually &lt;/del&gt;interest in understanding the forces or stresses involved &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the deformation of a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;material&lt;/del&gt;.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;via &lt;/ins&gt;Cameroon into Sudan. The &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;construction is not &lt;/ins&gt;well understood. The shear zone dates to a minimum of 640 Ma (million years in the past). Motion occurred alongside the zone through the break-up of Gondwanaland &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://www.wakewiki.de/index.php?title=How_You_Can_Sharpen_Kitchen_Shears_5_Easy_Methods professional landscaping shears] within &lt;/ins&gt;the Jurassic and Cretaceous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;periods&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Some &lt;/ins&gt;of the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;were &lt;/ins&gt;rejuvenated more than &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;as soon as &lt;/ins&gt;earlier than and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in the course of &lt;/ins&gt;the opening of the South Atlantic in the Cretaceous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;period&lt;/ins&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the Adamawa uplift, a put up-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic exercise has occurred alongside &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a lot &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;size &lt;/ins&gt;of the Cameroon line from 130 Ma to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;present&lt;/ins&gt;, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/ins&gt;be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ on this &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/ins&gt;is thinned in a relatively slim belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a &lt;/ins&gt;hundred &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;and &lt;/ins&gt;twenty km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;formerly &lt;/ins&gt;thought to increase eastward &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;only &lt;/ins&gt;to the Darfur &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;region &lt;/ins&gt;of western Sudan. It&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/ins&gt;now interpreted to extend into central and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;japanese &lt;/ins&gt;Sudan, with a complete &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;length &lt;/ins&gt;of 4,000 km. Within the Sudan, the shear zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/ins&gt;have acted as a structural barrier to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;improvement &lt;/ins&gt;of deep Cretaceous-Tertiary sedimentary basins &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the north of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;realm&lt;/ins&gt;. Objections to this idea are that the Bahr el Arab and Blue Nile rifts extend northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;this areas helps the theory. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://lunarishollows.wiki/index.php?title=User:MarcMoller0813 professional landscaping shears] &lt;/ins&gt;pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time study across the Central African Shear Zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the Adamawa area of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://rentry.co/29348-when-you-suspect-a-freon-problem Wood Ranger Power Shears website] [https://brogue.wiki/mw/index.php?title=Our_Picks_For_The_Very_Best_Pruning_Shears_For_Gardening_For_2025 Wood Ranger Power Shears price] Power Shears manual &lt;/ins&gt;planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;discipline studies&lt;/ins&gt;&amp;quot;. Pankhurst, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://gummipuppen-wiki&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;de/index&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;php?title=Benutzer&lt;/ins&gt;:&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;JuliusPak557552 Wood Ranger Power Shears USA] &lt;/ins&gt;[https://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;dev&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;neos.epss.ucla.edu/wiki&lt;/ins&gt;/index.php&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;?title=Why_It_s_Best_To_Personal_A_Pair_Of_Fine_Kitchen_Shears Wood Ranger Power Shears manual] [https:&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;/wiki.dulovic.tech/index.php/Since_We_Use_Non-linear_Artificial_Diffusion garden power shears&lt;/ins&gt;] &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Shears Robert J. (2008). West Gondwana: &lt;/ins&gt;pre-Cenozoic correlations &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/ins&gt;the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;A hundred and fifteen &lt;/ins&gt;(2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://rentry.co/50226-answers-about-flower-gardening professional landscaping shears] &lt;/ins&gt;Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, tectonics, financial geology, geohazards&lt;/ins&gt;,&amp;#160; [&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;https&lt;/ins&gt;://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;healthwiz&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;co&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;uk&lt;/ins&gt;/index.php?title=&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Now_Alligator_Shears_Are_Hydraulically_Actuated professional landscaping shears&lt;/ins&gt;] geosites and geoscientific &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;education &lt;/ins&gt;of each nation. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's charge-dependent resistance to a change in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;form &lt;/ins&gt;or to movement of its neighboring &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;parts &lt;/ins&gt;relative to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;each other&lt;/ins&gt;. For liquids, it corresponds to the informal concept of thickness; for &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;instance&lt;/ins&gt;, syrup has &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a better &lt;/ins&gt;viscosity than water. Viscosity is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;outlined &lt;/ins&gt;scientifically as a force multiplied by a time divided by an area. Thus its SI &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;items &lt;/ins&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the internal frictional &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;power &lt;/ins&gt;between &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;adjoining &lt;/ins&gt;layers of fluid which might be in relative movement. As an illustration, when a viscous fluid is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;pressured through &lt;/ins&gt;a tube, it flows extra &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shortly &lt;/ins&gt;close to the tube's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;center &lt;/ins&gt;line than near its partitions. Experiments present that some stress (&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;similar &lt;/ins&gt;to a stress distinction between the two ends of the tube) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;needed &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;maintain &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;circulate&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;It &lt;/ins&gt;is because a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;power &lt;/ins&gt;is required to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;beat &lt;/ins&gt;the friction between the layers of the fluid &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;which &lt;/ins&gt;are in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/ins&gt;. For a tube with a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;relentless rate &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;, the power of the compensating &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;drive &lt;/ins&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;In general, viscosity depends on a fluid's state, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;akin &lt;/ins&gt;to its temperature, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;stress&lt;/ins&gt;, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;price &lt;/ins&gt;of deformation. However, the dependence on a few of these properties is negligible in certain &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cases&lt;/ins&gt;. For instance, the viscosity of a Newtonian fluid doesn't &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;vary &lt;/ins&gt;considerably with the rate of deformation. Zero viscosity (no resistance to shear stress) is observed &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;solely &lt;/ins&gt;at very low temperatures in superfluids; in any other case, the second regulation of thermodynamics requires all fluids to have &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;positive &lt;/ins&gt;viscosity. A fluid that has zero viscosity (non-viscous) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is called splendid &lt;/ins&gt;or&amp;#160; [&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;http&lt;/ins&gt;://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;43&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;136.48.165:3003&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rhystravis1111&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;7732961&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;wiki/Following+the+Skirting+of+the+Fleece professional landscaping shears&lt;/ins&gt;] &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;inviscid. For non-Newtonian fluids' viscosity, &lt;/ins&gt;there are pseudoplastic, plastic, and dilatant flows which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/ins&gt;time-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;unbiased&lt;/ins&gt;, and there are thixotropic and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://www.wakewiki.de/index.php?title=Benutzer:DamienCarls0 professional landscaping shears] &lt;/ins&gt;rheopectic flows &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;which might be &lt;/ins&gt;time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum also referred to a viscous glue derived from mistletoe berries. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;materials &lt;/ins&gt;science and engineering, there is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;commonly &lt;/ins&gt;interest in understanding the forces or stresses involved &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the deformation of a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;fabric&lt;/ins&gt;.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>ShaynaCross</name></author>	</entry>

	<entry>
		<id>http://www.vokipedia.de/index.php?title=Central_African_Shear_Zone&amp;diff=104060&amp;oldid=prev</id>
		<title>VitoStallcup88 am 17. August 2025 um 04:12 Uhr</title>
		<link rel="alternate" type="text/html" href="http://www.vokipedia.de/index.php?title=Central_African_Shear_Zone&amp;diff=104060&amp;oldid=prev"/>
				<updated>2025-08-17T04:12:49Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class='diff diff-contentalign-left'&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 17. August 2025, 04:12 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea by Cameroon into Sudan. The structure &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is not nicely &lt;/del&gt;understood. The shear zone dates to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;at the very least &lt;/del&gt;640 Ma (million years in the past). Motion occurred alongside the zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;during &lt;/del&gt;the break-up of Gondwanaland &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the Jurassic and Cretaceous intervals. A few of the faults within the zone had been rejuvenated more than &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;as soon as before &lt;/del&gt;and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the opening of the South Atlantic in the Cretaceous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;period&lt;/del&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the Adamawa uplift, a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;submit&lt;/del&gt;-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;activity &lt;/del&gt;has occurred &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;along a lot &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;size &lt;/del&gt;of the Cameroon line from 130 Ma to the current, and could also be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;this &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/del&gt;is thinned in a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;comparatively &lt;/del&gt;slim belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;120 &lt;/del&gt;km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was previously thought to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;extend &lt;/del&gt;eastward solely to the Darfur area of western Sudan. It&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/del&gt;now interpreted to extend into central and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;jap &lt;/del&gt;Sudan, with a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;total &lt;/del&gt;size of 4,000 km. Within the Sudan, the shear zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;might &lt;/del&gt;have acted as a structural barrier to development of deep Cretaceous-Tertiary sedimentary basins &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the north of the area. Objections to this &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;concept &lt;/del&gt;are that the Bahr el Arab and Blue Nile rifts &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lengthen &lt;/del&gt;northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;this areas &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;supports &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;idea&lt;/del&gt;. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://carecall.co.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=1495931 cut thick branches easily] &lt;/del&gt;Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time study &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the Central African Shear Zone &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the Adamawa area of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; cordless [https://bbarlock.com/index.php/User:Heidi8824152 Wood Ranger Power Shears website] shears &lt;/del&gt;and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://online-learning-initiative.org/wiki/index.php/User:UHGMarshall cut thick branches easily] &lt;/del&gt;J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;field studies&lt;/del&gt;&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/del&gt;the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;One hundred fifteen &lt;/del&gt;(2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://wiki.learning4you.org/index.php?title=User:DarbyCarboni cut thick branches easily] &lt;/del&gt;Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;, tectonics&lt;/del&gt;,&amp;#160; [http://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;ttceducation&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;co&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;kr/bbs/board.php?bo_table=free&amp;amp;wr_id=2869872 Wood Ranger Power Shears warranty] [http://www.vokipedia.de&lt;/del&gt;/index.php?title=&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Garden_Shears_6_Inch_Pruning_Scissors_With_Teflon_Coating_Precision_Blades buy Wood Ranger Power Shears&lt;/del&gt;] &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Power Shears features financial &lt;/del&gt;geology, geohazards, geosites and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://lst.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=113252 cut thick branches easily] &lt;/del&gt;geoscientific &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;training &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;every country&lt;/del&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;rate&lt;/del&gt;-dependent resistance to a change in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;form &lt;/del&gt;or to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion &lt;/del&gt;of its neighboring portions relative to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;each other&lt;/del&gt;. For liquids, it corresponds to the informal &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;idea &lt;/del&gt;of thickness; for example, syrup has &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a better &lt;/del&gt;viscosity than water. Viscosity is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;outlined &lt;/del&gt;scientifically as a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/del&gt;multiplied by a time divided by an area. Thus its SI &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;items &lt;/del&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;inner &lt;/del&gt;frictional &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/del&gt;between adjacent layers of fluid which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;can &lt;/del&gt;be in relative movement. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;For instance&lt;/del&gt;, when a viscous fluid is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressured via &lt;/del&gt;a tube, it flows extra quickly close to the tube's middle line than &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;close to &lt;/del&gt;its partitions. Experiments present that some stress (&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;such as &lt;/del&gt;a stress distinction between the two ends of the tube) is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;needed &lt;/del&gt;to sustain the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;. This is because a force is required to overcome the friction between the layers of the fluid that are in relative &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/del&gt;. For a tube with a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;relentless charge &lt;/del&gt;of circulation, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://rentry.co/73038-discover-precision-cutting-with-top-quality-fabric-scissors Wood Ranger Power Shears shop] &lt;/del&gt;of the compensating &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://wiki.giroudmathias.ch/index.php?title=Choosing_The_Most_Effective_Power_Pruning_Shears Wood Ranger Power Shears review] &lt;/del&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Normally&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://andyfreund.de/wiki/index.php?title=3._A_Shearing_Machine;_A_Blade cut thick branches easily] &lt;/del&gt;viscosity &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is dependent upon &lt;/del&gt;a fluid's state, comparable to its temperature, pressure, and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;charge &lt;/del&gt;of deformation. However, the dependence on a few of these properties is negligible in certain &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cases&lt;/del&gt;. For &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;example&lt;/del&gt;, the viscosity of a Newtonian fluid doesn't &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;differ &lt;/del&gt;considerably with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;speed &lt;/del&gt;of deformation. Zero viscosity (no resistance to shear stress) is observed only at very low temperatures in superfluids; in any other case, the second &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;law &lt;/del&gt;of thermodynamics requires all fluids to have &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;positive &lt;/del&gt;viscosity. A fluid that has zero viscosity (non-viscous) &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is called excellent &lt;/del&gt;or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;can &lt;/del&gt;be time-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;unbiased&lt;/del&gt;, and there are thixotropic and rheopectic flows &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which might be &lt;/del&gt;time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum also referred to a viscous glue derived from mistletoe berries. In supplies science and engineering, there is usually &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;curiosity &lt;/del&gt;in understanding the forces or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://www.wakewiki.de/index.php?title=Benutzer:SusannahHooley5 cut thick branches easily] &lt;/del&gt;stresses involved &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the deformation of a material.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea by &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;means of &lt;/ins&gt;Cameroon into Sudan. The structure &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;just isn't well &lt;/ins&gt;understood. The shear zone dates to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a minimum of &lt;/ins&gt;640 Ma (million years in the past). Motion occurred alongside the zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/ins&gt;the break-up of Gondwanaland &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the Jurassic and Cretaceous intervals. A few of the faults within the zone had been rejuvenated more than &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;once earlier than &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/ins&gt;the opening of the South Atlantic in the Cretaceous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;interval&lt;/ins&gt;. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/ins&gt;the Adamawa uplift, a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;put up&lt;/ins&gt;-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;exercise &lt;/ins&gt;has occurred &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;alongside most &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;length &lt;/ins&gt;of the Cameroon line from 130 Ma to the current, and could also be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;on &lt;/ins&gt;this &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;space &lt;/ins&gt;is thinned in a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;relatively &lt;/ins&gt;slim belt, with the asthenosphere upwelling from a depth of about 190 km to about &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;one hundred twenty &lt;/ins&gt;km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was previously thought to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;increase &lt;/ins&gt;eastward solely to the Darfur area of western Sudan. It &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/ins&gt;now interpreted to extend into central and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;eastern &lt;/ins&gt;Sudan, with a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;complete &lt;/ins&gt;size of 4,000 km. Within the Sudan, the shear zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;could &lt;/ins&gt;have acted as a structural barrier to development of deep Cretaceous-Tertiary sedimentary basins &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the north of the area. Objections to this &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;idea &lt;/ins&gt;are that the Bahr el Arab and Blue Nile rifts &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;extend &lt;/ins&gt;northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;on &lt;/ins&gt;this areas &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;helps &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;theory&lt;/ins&gt;. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://wiki.monnaie-libre.fr/wiki/From_2025_By_2025 outdoor trimming tool] &lt;/ins&gt;G. W. (1986). &amp;quot;A teleseismic delay time study &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/ins&gt;the Central African Shear Zone &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the Adamawa area of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;subject research&lt;/ins&gt;&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://aeshma.net/index.php/Quality_Used_Machinery outdoor trimming tool] &lt;/ins&gt;pre-Cenozoic correlations &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/ins&gt;the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;115 &lt;/ins&gt;(2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy,&amp;#160; [http://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;wiki&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;wild-sau&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;com&lt;/ins&gt;/index.php?title=&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Thinning_Shears_Vs_Texturizing_Shears_-_Ask_A_Hairstylist outdoor trimming tool&lt;/ins&gt;] &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;tectonics, economic &lt;/ins&gt;geology, geohazards, geosites and geoscientific &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;schooling &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;each nation&lt;/ins&gt;. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt; &amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;charge&lt;/ins&gt;-dependent resistance to a change in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shape &lt;/ins&gt;or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://bbarlock.com/index.php/Expert_Collection_Man_Box outdoor trimming tool] &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement &lt;/ins&gt;of its neighboring portions relative to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;one another&lt;/ins&gt;. For liquids, it corresponds to the informal &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;concept &lt;/ins&gt;of thickness; for example, syrup has &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the next &lt;/ins&gt;viscosity than water. Viscosity is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;defined &lt;/ins&gt;scientifically as a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/ins&gt;multiplied by a time divided by an area. Thus its SI &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;units &lt;/ins&gt;are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;internal &lt;/ins&gt;frictional &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[https://koreanaggies.net/board_Lmao72/1920402 Wood Ranger Power Shears for sale] &lt;/ins&gt;between adjacent layers of fluid which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;might &lt;/ins&gt;be in relative movement. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;As an illustration&lt;/ins&gt;, when a viscous fluid is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;forced by way of &lt;/ins&gt;a tube, it flows extra quickly close to the tube's middle line than &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;near &lt;/ins&gt;its partitions. Experiments present that some stress (&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;corresponding to &lt;/ins&gt;a stress distinction between the two ends of the tube) is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;required &lt;/ins&gt;to sustain the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;stream&lt;/ins&gt;. This is because a force is required to overcome the friction between the layers of the fluid that are in relative &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;. For a tube with a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constant fee &lt;/ins&gt;of circulation, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;power &lt;/ins&gt;of the compensating &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;force &lt;/ins&gt;is proportional to the fluid's viscosity.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;In general&lt;/ins&gt;, viscosity &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;depends on &lt;/ins&gt;a fluid's state, comparable to its temperature, pressure, and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;fee &lt;/ins&gt;of deformation. However, the dependence on a few of these properties is negligible in certain &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;circumstances&lt;/ins&gt;. For &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;instance&lt;/ins&gt;, the viscosity of a Newtonian fluid doesn't &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;fluctuate &lt;/ins&gt;considerably with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rate &lt;/ins&gt;of deformation. Zero viscosity (no resistance to shear stress) is observed only at very low temperatures in superfluids; in any other case, the second &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;regulation &lt;/ins&gt;of thermodynamics requires all fluids to have &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constructive &lt;/ins&gt;viscosity. A fluid that has zero viscosity (non-viscous) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as ideally suited &lt;/ins&gt;or inviscid. For non-Newtonian fluids' viscosity, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://pipewiki.org/wiki/index.php/User:YukikoCorbitt8 outdoor trimming tool] &lt;/ins&gt;there are pseudoplastic, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://git.sparrowcomm.com/bradberg554612 outdoor trimming tool] &lt;/ins&gt;plastic, and dilatant flows which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;might &lt;/ins&gt;be time-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;independent&lt;/ins&gt;, and there are thixotropic and rheopectic flows &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;that are &lt;/ins&gt;time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum also referred to a viscous glue derived from mistletoe berries. In supplies science and engineering, there is usually &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;interest &lt;/ins&gt;in understanding the forces or stresses involved &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the deformation of a material.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
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		<summary type="html">&lt;p&gt;Die Seite wurde neu angelegt: „&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea by Cameroon into Sud…“&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Neue Seite&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea by Cameroon into Sudan. The structure is not nicely understood. The shear zone dates to at the very least 640 Ma (million years in the past). Motion occurred alongside the zone during the break-up of Gondwanaland within the Jurassic and Cretaceous intervals. A few of the faults within the zone had been rejuvenated more than as soon as before and throughout the opening of the South Atlantic in the Cretaceous period. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts throughout the Adamawa uplift, a submit-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic activity has occurred along a lot of the size of the Cameroon line from 130 Ma to the current, and could also be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ in this area is thinned in a comparatively slim belt, with the asthenosphere upwelling from a depth of about 190 km to about 120 km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was previously thought to extend eastward solely to the Darfur area of western Sudan. It's now interpreted to extend into central and jap Sudan, with a total size of 4,000 km. Within the Sudan, the shear zone might have acted as a structural barrier to development of deep Cretaceous-Tertiary sedimentary basins within the north of the area. Objections to this concept are that the Bahr el Arab and Blue Nile rifts lengthen northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts in this areas supports the idea. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux,  [http://carecall.co.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=1495931 cut thick branches easily] Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time study throughout the Central African Shear Zone within the Adamawa area of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes,  cordless [https://bbarlock.com/index.php/User:Heidi8824152 Wood Ranger Power Shears website] shears and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead,  [https://online-learning-initiative.org/wiki/index.php/User:UHGMarshall cut thick branches easily] J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential field studies&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations across the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure throughout the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. One hundred fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth,  [https://wiki.learning4you.org/index.php?title=User:DarbyCarboni cut thick branches easily] Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics,  [http://ttceducation.co.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=2869872 Wood Ranger Power Shears warranty] [http://www.vokipedia.de/index.php?title=Garden_Shears_6_Inch_Pruning_Scissors_With_Teflon_Coating_Precision_Blades buy Wood Ranger Power Shears] Power Shears features financial geology, geohazards, geosites and  [http://lst.kr/bbs/board.php?bo_table=free&amp;amp;wr_id=113252 cut thick branches easily] geoscientific training of every country. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's rate-dependent resistance to a change in form or to motion of its neighboring portions relative to each other. 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Zero viscosity (no resistance to shear stress) is observed only at very low temperatures in superfluids; in any other case, the second law of thermodynamics requires all fluids to have positive viscosity. A fluid that has zero viscosity (non-viscous) is called excellent or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows which can be time-unbiased, and there are thixotropic and rheopectic flows which might be time-dependent. The phrase &amp;quot;viscosity&amp;quot; is derived from the Latin viscum (&amp;quot;mistletoe&amp;quot;). Viscum also referred to a viscous glue derived from mistletoe berries. In supplies science and engineering, there is usually curiosity in understanding the forces or  [https://www.wakewiki.de/index.php?title=Benutzer:SusannahHooley5 cut thick branches easily] stresses involved in the deformation of a material.&amp;lt;br&amp;gt;&lt;/div&gt;</summary>
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