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- Tejas_sequence abstract "The Tejas sequence was the last major marine transgression across the North American 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 seas in North America; indeed, the Atlantic coast advanced only as far as the Mississippi Embayment. The Tejas was deeper in Eurasia and Africa, which experienced widespread 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.".
- Tejas_sequence wikiPageID "5723930".
- Tejas_sequence wikiPageRevisionID "544435648".
- Tejas_sequence hasPhotoCollection Tejas_sequence.
- Tejas_sequence subject Category:Geology_of_the_United_States.
- Tejas_sequence subject Category:Historical_geology.
- Tejas_sequence subject Category:Paleogene.
- Tejas_sequence comment "The Tejas sequence was the last major marine transgression across the North American 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 seas in North America; indeed, the Atlantic coast advanced only as far as the Mississippi Embayment.".
- Tejas_sequence label "Sequenza Tejas".
- Tejas_sequence label "Tejas sequence".
- Tejas_sequence sameAs Sequenza_Tejas.
- Tejas_sequence sameAs m.0f18f4.
- Tejas_sequence sameAs Q668931.
- Tejas_sequence sameAs Q668931.
- Tejas_sequence wasDerivedFrom Tejas_sequence?oldid=544435648.
- Tejas_sequence isPrimaryTopicOf Tejas_sequence.