Use of a regional, relict landscape to measure vertical deformation of the eastern Tibetan Plateau

Author:

Clark M. K.1,Royden L. H.1,Whipple K. X.1,Burchfiel B. C.1,Zhang X.2,Tang W.2

Affiliation:

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

2. Chengdu Institute of Geology and Mineral Resources; Chengdu China

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference73 articles.

1. Measurement of tectonic surface uplift rate in a young collisional mountain belt;Abbott;Nature,1997

2. Akciz , S. 2004 Structural and geochronological constraints on the ductile deformation observed along the Gaoligong Shan and Chong Shan shear zones, Yunnan (China) Mass. Inst. of Technol. Cambridge

3. Geometry, kinematics and regional significance of the Chong Shan shear zone, Yunnan, China;Akciz;Geol. Soc. Am. Abstr. Programs,2001

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

5. Physiographic history of the Yangtze;Barbour;Geogr. J.,1936

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