Evidence for an early-MORB to fore-arc evolution within the Zagros suture zone: Constraints from zircon U-Pb geochronology and geochemistry of the Neyriz ophiolite (South Iran)

Author:

Monsef Iman,Monsef Reza,Mata João,Zhang Zhiyong,Pirouz Mortaza,Rezaeian Mahnaz,Esmaeili Rasoul,Xiao Wenjiao

Funder

Chinese Academy of Sciences

National Natural Science Foundation of China

Institute for Advanced Studies in Basic Sciences

FCT

Publisher

Elsevier BV

Subject

Geology

Reference119 articles.

1. Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt–rock reactions;Ackerman;Chemical Geology,2009

2. Ultramafic and mafic cumulates from the Neyriz ophiolite complex in SE parts of the Zagros Range (Iran);Adib,1979

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. Obduction: why, how and where. Clues from analog models;Agard;Earth and Planetary Science Letters,2014

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