Oligo-Miocene exhumation of the Beni-Bousera peridotite through a lithosphere-scale extensional shear zone-Reference-Cited by-同舟云学术

Oligo-Miocene exhumation of the Beni-Bousera peridotite through a lithosphere-scale extensional shear zone

Published:2011-02 Issue:1 Volume:24 Page:49-60
ISSN:0985-3111
Container-title:Geodinamica Acta
language:en
Short-container-title:Geodinamica Acta

Author:

Afiri A.¹²,Gueydan F.¹,Pitra P.¹,Essaifi A.²,Précigout J.³

Affiliation:

1. a Géosciences Rennes , Université de Rennes 1 , CNRS UMR 6118, Rennes , France

2. b Département de Géologie, BP 2390, Faculté des Sciences Semlalia , 40000 , Marrakech , Morocco

3. c Department of Structural Geology and Tectonics , ETH-Zürich, Zürich , Switzerland

Publisher

Informa UK Limited

Subject

Earth-Surface Processes,Geophysics

Link

https://www.tandfonline.com/doi/pdf/10.3166/ga.24.49-60

Reference78 articles.

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2. The Ronda Peridotite: Garnet-, Spinel-, and Plagioclase-Lherzolite Facies and the P-T Trajectories of a High-Temprature Mantle Intrusion

3. Timing of tectonic events in the Alpujárride Complex, Betic Cordillera, southern Spain

4. Early Miocene continental subduction and rapid exhumation in the western Mediterranean

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