Geochemical and geochronological constraints on the origin of the Sabzevar ophiolites (NE Iran): forced far-field subduction initiation in the upper-plate of the Neo-Tethys subduction zone-Reference-Cited by-同舟云学术

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Geochemical and geochronological constraints on the origin of the Sabzevar ophiolites (NE Iran): forced far-field subduction initiation in the upper-plate of the Neo-Tethys subduction zone

Published:2023-05 Issue:2 Volume:83 Page:125962
ISSN:0009-2819
Container-title:Geochemistry
language:en
Short-container-title:Geochemistry

Author:

Nasrabady Mohsen,Shi Yuruo,Lustrino Michele,Rossetti Federico

Funder

Imam Khomeini International University

National Natural Science Foundation of China

Ministero dell’Istruzione, dell’Università e della Ricerca

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference158 articles.

1. Zagros orogeny: a subduction-dominated process;Agard;Geol. Mag.,2011

2. The subduction plate interface: rock record and mechanical coupling (from long to short timescales);Agard;Lithos,2018

3. Geological map of Iran sheet 7662-Soltanabad, scale 1:100,000;Akrami,2000

4. Tectonic of Zagros orogenic belt of Iran: new data and interpretations;Alavi;Tectonophysics,1994

5. U-Pb zircon ages, field geology and geochemistry of the Kermanshah ophiolite (Iran): from continental rifting at 79 Ma to oceanic core complex at ca. 36 Ma in the southern Neo-tethys;Ao;Gondwana Res.,2016

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1. Geochemistry, Sr-Nd isotopes and zircon U-Pb dating of magmatic rocks from the Talesh range, western Alborz: New insights into Late Cretaceous evolution of the southern Eurasian margin;Geochemistry;2023-11

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