The Plio-Quaternary permeable bodies of the Mamora (Morocco).: Geometry and structural influences.

被引：9

作者：

Zouhri, L

Lamouroux, C

Vachard, D

Piqué, A

机构：

[1] Univ Artois, Fac Sci Jean Perrin, Equipe HSE, LAMH,Lab Hydrogeol, F-62307 Lens, France

[2] Univ Sci & Tech Lille Flandres Artois, Lab Geol Struct & Geodynam, F-59655 Villeneuve Dascq, France

[3] Univ Sci & Tech Lille Flandres Artois, CNRS, Upresa 8014, Lab Paleontol, F-59655 Villeneuve Dascq, France

[4] Inst UnivEuropeen Mer, UMR 6538, F-29280 Plouzane, France

来源：

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | 2001年 / 332卷 / 01期

关键词：

geometry; faults; permeable; aquifer; Mamora; geodynamics; Morocco;

D O I：

10.1016/S1251-8050(00)01493-2

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The geometrical configuration of the western Mamora basin highlighted a partition in horsts and grabens in the southern part and a system of three geological units (U1, U2, and U3) in the northern part. Two great structures have been deduced from this study: (1) the Rabat-Kenitra fault belonging to the 'sheared West-Mesetian zone' family, (2) the K2S fault depending of the important Hercynian Rabat-Tiflete fault. The depressions identified in the Mamora contain the Pliocene aquifer formations which overlay the impermeable Mio-Pliocene blue marls. (C) 2001 Academie des sciences / Editions scientifiques et medicales Elsevier SAS.

引用

页码：1 / 4

页数：4

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