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Key Laboratory of Continental Collision and Plateau Uplifting, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA Laboratory of Continental Collision and Plateau uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 18 Shuang Qing Road, Beijing 100085, China
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
A comment on “Orogen-parallel, active left-slip faults in the eastern Himalaya: Implications for the growth mechanism of the Himalayan arc” by Li and Yin (Earth Planet Sci. Lett. 274 (2008) 258-267)
Co-seismic ruptures of the 12 May 2008, Ms 8.0 Wenchuan earthquake, Sichuan: East-west crustal shortening on oblique, parallel thrusts along the eastern edge of Tibet
Early Mesozoic high pressure metamorphism in the Lhasa Block, Tibet: Implications for the growth of the Cimmerian subcontinent
Mid-Eocene high Sr/Y granites in the Northern Himalayan Gneiss Domes: Melting thickened lower continental crust
The effect of slip variability on earthquake slip-length scaling
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