Age and environments of the Red beds at Anoual (Middle Jurassic and Lower Cretaceous, eastern High Atlas, Morocco)

被引：19

作者：

Haddoumi, H ^{[1
]}

Almeras, Y

Bodergat, AM

Charriere, A

Mangold, C

Benshili, K

机构：

[1] Univ Mohamed, Fac Sci, Dept Geol, Oujda, Morocco

[2] Univ Lyon 1, UFR Sci Terre, F-69622 Villeurbanne, France

[3] Univ Lyon 1, UMR 5565, F-69622 Villeurbanne, France

[4] Univ Toulouse 3, CNRS, URA 1405, Lab Stratig Sequentielle & Micropaleontol, F-31062 Toulouse, France

[5] Ecole Natl Ind Minerale, Dept Geol, Rabat, Morocco

来源：

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | 1998年 / 327卷 / 02期

关键词：

red beds; brachiopods; ostracods; unconformities; Bathonian; Lower Cretaceous; High Atlas; Morocco;

D O I：

10.1016/S1251-8050(98)80043-8

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Lithology, sedimentology and palaeoenvironments allow a lithostratigraphic subdivision of the Red beds into five formations. A marine episode identified near the top of the first formation is Early Bathonian in age. An erosional unconformity overlies this marine level just below the Lower Cretaceous deposits. It could be related to a large sedimentary gap between the Lower Bathonian and the Lower Cretaceous series. (C) Academie des sciences / Elsevier, Paris.).

引用

页码：127 / 133

页数：7

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