Evolution of the Urgonian platform between the Jura and the Septentrional Subalpine Chains (France, Switzerland)

被引:16
作者
Charollais, J
Clavel, B
Schroeder, R
Busnardo, R
Decrouez, D
Cherchi, A
机构
[1] Univ Geneva, Dept Geol & Paleontol, CH-1211 Geneva 4, Switzerland
[2] Dept Sci Terre, F-69622 Villeurbanne, France
[3] Inst Geol Palaontol, D-60054 Frankfurt, Germany
[4] Museum Hist Nat, Dept Geol & Paleontol, CH-1211 Geneva 6, Switzerland
[5] Dipartimento Sci Terra, I-09100 Cagliari, Italy
关键词
France; Switzerland; southern Jura; Saleve; Northern Subalpine Chains; Urgonian; carbonate platform;
D O I
10.1016/j.geobios.2003.03.003
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The stratigraphic study of the Urgonian carbonate platform presented here was carried out on a directed transversal NW-SE and passing by Geneva. This transversal extends on 100 km length; it lies between the face of the "folded Jura" (Champagnole, the Jura) and the septentrional subalpine chains (Aravis, Haute-Savoie). Essentially based on the biostratigraphy (ammonites, orbitolinids, echinids) and on sequence stratigraphy, this study illustrates the progradation of the Urgonian platform from the "folded Jura" (top of the Lower Hauterivian) to the Aravais chain (lowermost Barremian). (C) 2003 Editions scientifiques et medicales Elsevier SAS. Tons droits reserves.
引用
收藏
页码:665 / 674
页数:10
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