Age, geochemistry, and emplacement of the ~40-Ma Baneh granite–appinite complex in a transpressional tectonic regime, Zagros suture zone, northwest Iran-Reference-Cited by-同舟云学术

Age, geochemistry, and emplacement of the ~40-Ma Baneh granite–appinite complex in a transpressional tectonic regime, Zagros suture zone, northwest Iran

Published:2018-01-12 Issue:2 Volume:61 Page:195-223
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Azizi Hossein¹^ORCID,Hadad Sepideh²,Stern Robert J.³,Asahara Yoshihiro⁴

Affiliation:

1. Mining Department, Faculty of Engineering, University of Kurdistan, Sanandaj, Iran

2. Earth Sciences Department, Faculty of Basic Sciences, University of Kurdistan, Sanandaj, Iran

3. Geosciences Department, University of Texas at Dallas, Richardson, TX, USA

4. Department of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan

Funder

Japan Society for the Promotion of Science

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2017.1422394

Reference101 articles.

1. Zircon U–Pb ages and geochemistry of Devonian A-type granites in the Iraqi Zagros Suture Zone (Damamna area): New evidence for magmatic activity related to the Hercynian orogeny

2. The role of extensional tectonics at different crustal levels on granite ascent and emplacement: an example from Tuscany (Italy)

3. Zagros orogeny: a subduction-dominated process

4. Tectonostratigraphic evolution of the Zagrosides of Iran

5. Tectonics of the zagros orogenic belt of iran: new data and interpretations

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