Structural setting and ophiolitic nature of Jurassic basic rocks associated with the Maghrebian flyschs in the Rif (Morocco) and Sicily (Italy).

被引：130

作者：

Durand-Delga, M ^{[1
]}

Rossi, P

Olivier, P

Puglisi, D

机构：

[1] La Pelisserie, F-81150 Florentin, France

[2] Bur Rech Geol & Minieres, F-45060 Orleans 02, France

[3] CNRS, UMR 5563, Equipe Petrophys Tecton & Geomorphol, F-31400 Toulouse, France

[4] Univ Toulouse 3, F-31400 Toulouse, France

[5] Univ Catania, Dipartimento Sci Geol, I-95129 Catania, Italy

来源：

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | 2000年 / 331卷 / 01期

关键词：

ophiolite; Maghrebides; Rif; Sicily; Predorsalian zone; Mauretanian flysch; Massylian flysch;

D O I：

10.1016/S1251-8050(00)01378-1

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

At both ends of the Maghrebides belt, in the Rif Mountains and Sicily, Middle to Upper Jurassic slices of basic rocks with an E-MORB character are associated with various tectonic units of the Maghrebian flysch zone. This zone, which was located between the internal zones, originally linked to the European plate and the African external zones of this Alpine belt, was therefore oceanized, at least partially, and acted as a transform fault between the mid Atlantic and the Ligurian ocean, both of them being open at that time. (C) 2000 Academie des sciences /Editions scientifiques et medicales Elsevier SAS.

引用

页码：29 / 38

页数：10

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