Petrological evidence for stepwise accretion of metamorphic soles during subduction infancy (Semail ophiolite, Oman and UAE)

Author:

Soret Mathieu1ORCID,Agard Philippe12ORCID,Dubacq Benoît1ORCID,Plunder Alexis13ORCID,Yamato Philippe24ORCID

Affiliation:

1. Sorbonne Universités; UPMC Univ. Paris 06; CNRS; Institut des Sciences de la Terre de Paris (ISTeP); Paris France

2. Institut Universitaire de France; Paris France

3. Department of Earth Sciences; Utrecht University; Utrecht The Netherlands

4. Géosciences Rennes; Université de Rennes 1; CNRS UMR 6118; Rennes Cedex France

Funder

Agence Nationale de la Recherche

Institut Universitaire de France

H2020 European Research Council

ONLAP

ERC SINK

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Reference97 articles.

1. Crustal stacking and expulsion tectonics during continental subduction: P-T deformation constraints from Oman;Agard;Tectonics,2010

2. Plate interface rheological switches during subduction infancy: Control on slab penetration and metamorphic sole formation;Agard;Earth and Planetary Science Letters,2016

3. The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex;Alabaster;Contribution to Mineralogy and Petrology,1982

4. The ophiolite-radiolarite belt of the North-Oman Mountains;Allemann;Eclogae Geologicae Helvetiae,1972

5. Raman spectra of carbonaceous material in metasediments: A new geothermometer;Beyssac;Journal of Metamorphic Geology,2002

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