Metamorphic evolution of (ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen (Central Asian Orogenic Belt): Geodynamic implications

2015 ◽  
Vol 28 (1) ◽  
pp. 1-25 ◽  
Author(s):  
Reiner Klemd ◽  
Jun Gao ◽  
Ji-Lei Li ◽  
Melanie Meyer
Keyword(s):  
High Pressure ◽  
Orogenic Belt ◽  
Central Asian Orogenic Belt ◽  
The South ◽  
Metamorphic Evolution ◽  
Ultra High Pressure ◽  
Central Asian ◽  
South Tianshan

Late Paleozoic subduction and collision processes during the amalgamation of the Central Asian Orogenic Belt along the South Tianshan suture zone

Lithos ◽  
2016 ◽  
Vol 246-247 ◽  
pp. 1-12 ◽  
Author(s):  
Yigui Han ◽  
Guochun Zhao ◽  
Min Sun ◽  
Paul R. Eizenhöfer ◽  
Wenzhu Hou ◽  
...  
Keyword(s):  
Suture Zone ◽  
Orogenic Belt ◽  
Central Asian Orogenic Belt ◽  
Late Paleozoic ◽  
The South ◽  
Central Asian ◽  
South Tianshan ◽  
Collision Processes

scholarly journals High-pressure mafic granulites of the South Muya Block (Central Asian Orogenic Belt)

2017 ◽  
Vol 473 (2) ◽  
pp. 423-426 ◽  
Author(s):  
S. Yu. Skuzovatov ◽  
V. S. Shatsky ◽  
S. I. Dril
Keyword(s):  
High Pressure ◽  
Orogenic Belt ◽  
Central Asian Orogenic Belt ◽  
The South ◽  
Central Asian

Deformation Analysis and Tectonic Implications of South Tianshan Orogenic Belt, SW China

2014 ◽  
Vol 1010-1012 ◽  
pp. 1404-1407
Author(s):  
Hui Mei Guan ◽  
Hai Yan Cheng ◽  
Yan Li Kang
Keyword(s):  
Tectonic Evolution ◽  
Orogenic Belt ◽  
High Temperature Deformation ◽  
Temperature Deformation ◽  
Deformation Analysis ◽  
The South ◽  
West China ◽  
Central Asian ◽  
Tianshan Orogenic Belt ◽  
South Tianshan

The Tianshan Orogenic Belt, which is located in the southwestern part of the Central Asian Orogenic Belt (CAOB), is an important component in the reconstruction of the tectonic evolution of the CAOB. In order to examine the evolution of the Tianshan Orogenic Belt, we performed macroscopic, microscopic structure observations analyses with deformed rocks along orogen-perpendicular transects pass Wuwamen in the South Tianshan orogenic belt of south west China, and we propose that the South Tianshan Orogenic belt enterwent a high temperature deformation in Wuwamen area during the plate interactions in Late Paleozoic.

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