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From Tethyan subduction to Arabia-Eurasia continental collision: Multiple geo-thermochronological signals from granitoids in NW Iran

  • Published:2023-07 Issue: Volume:621 Page:111567
  • ISSN:0031-0182
  • Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
  • language:en
  • Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Zhang Zhiyong,Zack Thomas,Kohn Barry,Malusà Marco G.,Wu Lin,Rezaeian Mahnaz,Wang Nan,Xiang Dunfeng,Guo Chao,Esmaeili Rasoul,Wan Bo,Xiao Wenjiao

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference161 articles.

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

2. Far-field tectonic effects of the Arabia-Eurasia collision and the inception of the North Anatolian Fault system;Albino;Geol. Mag.,2014

3. Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates;Allen;Tectonics,2004

4. Discussion on the Eocene bimodal Piranshahr massif of the Sanadaj-Sirjan Zone, West Iran: a marker of the end of collision in the Zagros orogen;Allen;J. Geol. Soc.,2009

5. Arabia-Eurasia collision and the forcing of mid-Cenozoic global cooling;Allen;Paleogeogr. Paleoclimatol. Paleoecol.,2008

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