Textural evolution during high-pressure dehydration of serpentinite to peridotite and its relation to stress orientations and kinematics of subducting slabs: Insights from the Almirez ultramafic massif-Reference-Cited by-同舟云学术

Textural evolution during high-pressure dehydration of serpentinite to peridotite and its relation to stress orientations and kinematics of subducting slabs: Insights from the Almirez ultramafic massif

Published:2018-11 Issue: Volume:320-321 Page:470-489
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Dilissen Nicole,Hidas Károly,Garrido Carlos J.,Kahl Wolf-Achim,López Sánchez-Vizcaíno Vicente,Padrón-Navarta José Alberto

Funder

EU-FP7 Marie Curie Initial Training Network

Ministry of Economy, Industry, and Competitiveness

Junta de Andalucía research groups

DFG Reinhart Koselleck

MINECO and the State Research Agency

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference91 articles.

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2. Deformation mechanisms and rheology of serpentines in experiments and in nature;Amiguet;Journal of Geophysical Research: Solid Earth,2014

3. Numerical simulations of subduction zones - effect of slab dehydration on the mantle wedge dynamics;Arcay;Physics of the Earth and Planetary Interiors,2005

4. Exhumation, doming and slab retreat in the Betic Cordillera (SE Spain): in situ Ar-40/Ar-39 ages and P-T-d-t paths for the Nevado-Filabride complex;Augier;Journal of Metamorphic Geology,2005

5. Deformation mechanisms of antigorite serpentinite at subduction zone conditions determined from experimentally and naturally deformed rocks;Auzende;Earth and Planetary Science Letters,2015

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