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Geochemistry of Precambrian ophiolites from Bou Azzer, Morocco

Identifieur interne : 000513 ( France/Analysis ); précédent : 000512; suivant : 000514

Geochemistry of Precambrian ophiolites from Bou Azzer, Morocco

Auteurs : J. L. Bodinier [France] ; C. Dupuy [France] ; J. Dostal [Canada]

Source :

RBID : ISTEX:616E536C1BCD9C7CCAAF579E93114D998603D6AB

Abstract

Abstract: The Upper Proterozoic ophiolite complex of Bou Azzer, Morocco, includes ultramafic rocks, cumulate gabbros, sheeted dykes, pillow lavas and diorite-quartz diorite intrusions and an overlying volcano-sedimentary sequence. The gabbroic cumulates, basaltic flows and dykes have compositions similar to recent ocean-floor rocks (N- and/or T-type). Among other features, they have comparable light REE-depleted patterns and relations of Ti-Zr and La-Nb. Although fractional crystallization played an important role in the evolution of these rocks, the large variations in their chemical compositions require generation from a heterogeneous upper mantle source and/or by a dynamic partial melting process. Diorites, quartz diorites and the volcanic rocks of the overlying sequence are calc-alkaline, genetically unrelated to the tholeiitic suite and indicative of an island arc setting. A possible tectonic model for the ophiolite complex is a marginal basin just behind a still active island arc.

Url:
DOI: 10.1007/BF00371401


Affiliations:


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ISTEX:616E536C1BCD9C7CCAAF579E93114D998603D6AB

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