Two phases of Mesozoic north-south extension in the eastern Altyn Tagh range, northern Tibetan Plateau

Author:

Chen Xuanhua1,Yin An2,Gehrels George E.3,Cowgill Eric S.2,Grove Marty2,Harrison T. Mark2,Wang Xiao-Feng1

Affiliation:

1. Institute of Geomechanics; Chinese Academy of Geological Sciences; Beijing; China

2. Department of Earth and Space Sciences; University of California; Los Angeles; California; USA

3. Department of Geosciences; University of Arizona; Tucson; Arizona; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference66 articles.

1. Structure and evolution of the Himalayan-Tibet orogenic belt;Allègre;Nature,1984

2. Intracrustal detachment with zones of continental deformation;Burchfiel;Geology,1989

3. Geological and geophysical evidence for deep subduction of continental crust beneath the Pamir;Burtman;Spec. Pap. Geol. Soc. Am.,1993

4. Tectonic features of the Mount Jolmo Lungma region in southern Tibet, China;Chang;Sci. Geol. Sin.,1973

5. The age of the Altun granulite facies complex and the basement of the Tarim basin;Che;Reg. Geol. China.,1996

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