Late Cenozoic evolution of the eastern margin of the Tibetan Plateau: Inferences from40Ar/39Ar and (U-Th)/He thermochronology-Reference-Cited by-同舟云学术

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Late Cenozoic evolution of the eastern margin of the Tibetan Plateau: Inferences from40Ar/39Ar and (U-Th)/He thermochronology

Published:2002-01 Issue:1 Volume:21 Page:1-1-1-20
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Kirby Eric¹,Reiners Peter W.²,Krol Michael A.³,Whipple Kelin X.¹,Hodges Kip V.¹,Farley Kenneth A.⁴,Tang Wenqing⁵,Chen Zhiliang⁵

Affiliation:

1. Department of Earth, Atmospheric, and Planetary Science; Massachusetts Institute of Technology; Cambridge Massachusetts USA

2. Department of Geology; Washington State University; Pullman Washington USA

3. Department of Earth Sciences; Boston University, Boston; Boston Massachusetts USA

4. Department of Geological and Planetary Sciences; California Institute of Technology; Pasadena California USA

5. Chengdu Institute of Geology and Mineral Resources; Chengdu Sichuan P.R. China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference89 articles.

1. Quaternary extension in southern Tibet: Field observations and tectonic implications;Armijo;J. Geophys. Res.,1986

2. High cooling and denudation rates at Kongur Shan, Eastern Pamir (Xinjiang, China) revealed by 40Ar/39Ar alkali feldspar thermochronology;Arnaud;Tectonics,1993

3. Differential exhumation in response to episodic thrusting along the eastern margin of the Tibetan Plateau;Arne;Tectonophysics,1997

4. Kinematic model of active deformation in Central Asia;Avouac;Geophys. Res. Lett.,1993

5. Erosional control of active compressional orogens

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