Major transgression during Late Cretaceous constrained by basin sediments in northern Africa: implication for global rise in sea level-Reference-Cited by-同舟云学术

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Major transgression during Late Cretaceous constrained by basin sediments in northern Africa: implication for global rise in sea level

Published:2017-07-06 Issue:4 Volume:11 Page:740-750
ISSN:2095-0195
Container-title:Frontiers of Earth Science
language:en
Short-container-title:Front. Earth Sci.

Author:

An Kaixuan,Chen Hanlin,Lin Xiubin,Wang Fang,Yang Shufeng,Wen Zhixin,Wang Zhaoming,Zhang Guangya,Tong Xiaoguang

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/article/10.1007/s11707-017-0661-0/fulltext.html

Reference77 articles.

1. Adatte T, Keller G, Stinnesbeck W (2002). Late Cretaceous to early Paleocene climate and sea-level fluctuations: the Tunisian record. Palaeogeogr Palaeoclimatol Palaeoecol, 178(3–4): 165–196

2. Bachmann M, Hirsch F (2006). Lower Cretaceous carbonate platform of the eastern Levant (Galilee and the Golan Heights): stratigraphy and second-order sea-level change. Cretac Res, 27(4): 487–512

3. Badalini G, Redfern J, Carr I D (2002). A synthesis of current understanding of the structural evolution of North Africa. J Pet Geol, 25(3): 249–258

4. Barbero L, Teixell A, Arboleya M L, Río P, Reiners P W, Bougadir B (2007). Jurassic-to-present thermal history of the central High Atlas (Morocco) assessed by low-temperature thermochronology. Terra Nova, 19(1): 58–64

5. Berner R A (1992). Palaeo-CO2 and climate. Nature, 358(6382): 114

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