http://debianws.lexgopc.com/wiki143/index.php?action=history&feed=atom&title=Tejas_sequenceTejas sequence - Revision history2026-05-14T19:51:07ZRevision history for this page on the wikiMediaWiki 1.43.1http://debianws.lexgopc.com/wiki143/index.php?title=Tejas_sequence&diff=3054400&oldid=previmported>AhmedElMohamedi at 18:36, 6 March 20252025-03-06T18:36:31Z<p></p>
<p><b>New page</b></p><div>{{Short description|Last major marine transgression across the North American craton}}<br />
The '''Tejas sequence''' was the last major marine [[Transgression (geology)|transgression]] across the [[North America]]n [[craton]]. Following the late [[Cretaceous]] regression that ended the [[Zuñi sequence]], the oceans advanced again early in the [[Cenozoic]], peaking during the [[Paleocene]] and [[Eocene]] epochs. There were no dramatic [[Epeiric Sea|epeiric seas]] in [[North America]]; indeed, the [[Atlantic Ocean|Atlantic coast]] advanced only as far as the [[Mississippi Embayment]].<ref name="Stanley">{{cite book |last1=Stanley |first1=Steven M. |title=Earth system history |date=1998 |publisher=W.H. Freeman |location=New York |isbn=0716728826 |page=516}}</ref><ref>{{cite book |last1=Monroe |first1=James S. |title=The changing earth : exploring geology and evolution |date=1997 |publisher=Wadsworth Pub |location=Belmont, Calif. |isbn=0314095772 |page=643 |edition=2nd}}</ref> The Tejas was deeper in [[Eurasia]] and [[Africa]], which experienced widespread [[Carbonate rock|carbonate]] deposition during the Eocene. There was a final transgression before the end of the [[Oligocene]], the end of which marked the end of the Tejas sequence.<ref name=Stanley/><br />
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==See also==<br />
*[[Cratonic sequence]]<br />
*[[Sequence stratigraphy]]<br />
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==References==<br />
{{reflist}}<br />
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[[Category:Historical geology]]<br />
[[Category:Geology of the United States]]<br />
[[Category:Paleogene geology]]<br />
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{{paleogene-stub}}<br />
{{palaeo-geo-stub}}</div>imported>AhmedElMohamedi