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La sequenza Tejas fu l'ultima trasgression … La sequenza Tejas fu l'ultima trasgressione marina attraverso il cratone del Nord America. Seguendo la regressione del tardo Cretaceo che pose fine alla Sequenza Zuñi, gli oceani avanzarono nuovamente in prossimità del Cenozoico, innalzandosi durante le epoche del Paleocene ed Eocene. Non ci furono drammatici nel Nord America; invero, la costa atlantica avanzò soltanto così lontano come l'. La Tejas fu più profonda in Eurasia e Africa, che sperimentò l'estesa sedimentazione del carbonato durante l'Eocene. Ci fu un'ultima trasgressione prima della fine dell'Oligocene che segnò la fine della sequenza Tejas.ne che segnò la fine della sequenza Tejas.
, The Tejas sequence was the last major mari … 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.hich marked the end of the Tejas sequence.
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| rdfs:comment |
La sequenza Tejas fu l'ultima trasgression … La sequenza Tejas fu l'ultima trasgressione marina attraverso il cratone del Nord America. Seguendo la regressione del tardo Cretaceo che pose fine alla Sequenza Zuñi, gli oceani avanzarono nuovamente in prossimità del Cenozoico, innalzandosi durante le epoche del Paleocene ed Eocene. Non ci furono drammatici nel Nord America; invero, la costa atlantica avanzò soltanto così lontano come l'. La Tejas fu più profonda in Eurasia e Africa, che sperimentò l'estesa sedimentazione del carbonato durante l'Eocene. Ci fu un'ultima trasgressione prima della fine dell'Oligocene che segnò la fine della sequenza Tejas.ne che segnò la fine della sequenza Tejas.
, The Tejas sequence was the last major mari … 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.hich marked the end of the Tejas sequence.
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Sequenza Tejas
, Tejas sequence
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