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・ Tejapur Landanpur
・ Tejar
・ Tejara
・ Tejarat Aria Gostar Iranian Navid Company
・ Tejarat Bank
・ Tejarat-e-Farda
・ Tejas
・ Tejas (album)
・ Tejas Airlines
・ Tejas and Jayhawk
・ Tejas Chavan
・ Tejas Club
・ Tejas Lake
・ Tejas Networks
・ Tejas Patel
Tejas sequence
・ Tejashree
・ Tejashree Pradhan Ketkar
・ Tejashwi Yadav
・ Tejashwini Gowda
・ Tejaswi Madivada
・ Tejaswi Prakash Wayangankar
・ Tejaswini Kolhapure
・ Tejaswini Pandit
・ Tejaswini Sawant
・ Tejat
・ Tejate
・ Tejay Johnson
・ Tejay van Garderen
・ Tejay, Kentucky


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Tejas sequence : ウィキペディア英語版
Tejas sequence
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.〔Stanley, Steven M. ''Earth System History''. New York: W.H. Freeman and Company, 1999. ISBN 0-7167-2882-6 pp. 516〕〔Monroe, James S., and Reed Wicander. ''The Changing Earth: Exploring Geology and Evolution'', 2nd ed. Belmont: West Publishing Company, 1997. ISBN 0-314-09577-2 pp. 643〕 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.〔
==See also==

*Cratonic sequence
*Sequence stratigraphy

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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