Low‐Temperature Thermochronology of the Chatkal‐Kurama Terrane (Uzbekistan‐Tajikistan): Insights Into the Meso‐Cenozoic Thermal History of the Western Tian Shan-Reference-Cited by-同舟云学术

Low‐Temperature Thermochronology of the Chatkal‐Kurama Terrane (Uzbekistan‐Tajikistan): Insights Into the Meso‐Cenozoic Thermal History of the Western Tian Shan

Published:2018-10 Issue:10 Volume:37 Page:3954-3969
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Jepson Gilby¹^ORCID,Glorie Stijn¹,Konopelko Dmitry²³,Gillespie Jack¹^ORCID,Danišík Martin⁴,Mirkamalov Rustam⁵^ORCID,Mamadjanov Yunus⁶⁷^ORCID,Collins Alan S.¹^ORCID

Affiliation:

1. Centre for Tectonics, Resources, and Exploration (TRaX), Department of Earth Sciences The University of Adelaide Adelaide Australia

2. Department of Geology and Geophysics Saint Petersburg State University Saint Petersburg Russia

3. Department of Geology and Geophysics Novosibirsk State University Novosibirsk Russia

4. John de Laeter Centre, TIGeR, School of Earth and Planetary Sciences Curtin University Perth Australia

5. State Committee of the Republic of Uzbekistan on Geology and Mineral Resources Tashkent Uzbekistan

6. Institute of Geology, Earthquake Engineering and Seismology Academy of Sciences of the Republic of Tajikistan Dushanbe Tajikistan

7. Research Center for Ecology and Environment of Central Asia (Dushanbe) Chinese Academy of Sciences‐Tajik Academy of Sciences Dushanbe Tajikistan

Funder

Ministry of Education and Science of the Russian Federation

Saint Petersburg State University

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2017TC004878

Reference75 articles.

1. Ahmedov N.(2000). ‘Stratified and intrusive formations of Uzbekistan’ Uzbekistan Geological Survey.

2. When and where did India and Asia collide?

3. Middle to Late Ordovician arc system in the Kyrgyz Middle Tianshan: From arc-continent collision to subsequent evolution of a Palaeozoic continental margin

4. Basin evolution within and adjacent to the Tien Shan Range, NW China

5. Cenozoic palaeoenvironmental and tectonic controls on the evolution of the northern Fergana Basin

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