Evidence for Paleocene–Eocene evolution of the foot of the Eurasian margin (Kermanshah ophiolite, SW Iran) from back-arc to arc: Implications for regional geodynamics and obduction-Reference-Cited by-同舟云学术

Evidence for Paleocene–Eocene evolution of the foot of the Eurasian margin (Kermanshah ophiolite, SW Iran) from back-arc to arc: Implications for regional geodynamics and obduction

Published:2013-12 Issue: Volume:182-183 Page:11-32
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Whitechurch H.,Omrani J.,Agard P.,Humbert F.,Montigny R.,Jolivet L.

Funder

MEBE programme (CNRS-University Pierre and Marie Curie of Paris-Consortium of oil companies)

Geological Survey of Iran

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference103 articles.

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3. Plate acceleration: the obduction trigger?;Agard;Earth and Planetary Science Letters,2007

4. Zagros orogeny: a subduction-dominated process;Agard;Geological Magazine,2011

5. The Maden Complex, SE Turkey: evolution of a Neotethyan continental margin;Aktas,1984

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