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Creator:: Shi, Xuhua, Kirby, Eric, Furlong, Kevin P., Meng, Kai, Robinson, Ruth, and Wang, Erchie
Abstract:: Controversial end member models for the growth and evolution of the Tibetan Plateau demand quantitative constraints of the lithospheric rheology. Direct determinations of bulk crustal rheology, however, remain relatively sparse. Here we use the flexural rebound of lacustrine shorelines developed during the Lingtong highstand around Siling Co, in central Tibet,...
Full Text:: , Eric Kirby, Kevin 128 P. Furlong, Kai Meng, Ruth Robinson and Erchie Wang. Earth and Planetary

Creator:: Shi, Xuhua, Kirby, Eric, Lu, Haijian, Robinson, Ruth, Furlong, Kevin P., and Wang, Erchie
Abstract:: Although geodetic measurements of interseismic deformation in interior Tibet suggest slow strain accumulation, active slip along the right-lateral Gyaring Co Fault is suggested to be between 8 and 21 mm/yr. Reliable geologic constraints on the slip rate along this fault are sparse. Here we document 12 ± 2 m of...
Full Text:: , central Tibet Holocene slip rate along the Gyaring Co Fault, central Tibet Shi, X., Kirby, E., Lu, H

Creator:: Shi, Xuhua, Kirby, Eric, Furlong, Kevin P., Meng, Kai, Robinson, Ruth, and Wang, Erchie
Abstract:: Controversial end member models for the growth and evolution of the Tibetan Plateau demand quantitative constraints of the lithospheric rheology. Direct determinations of bulk crustal rheology, however, remain relatively sparse. Here we use the flexural rebound of lacustrine shorelines developed during the Lingtong highstand around Siling Co, in central Tibet,...
Full Text:: from Holocene shoreline deflection around Siling Co Shi, X., Kirby, E., Furlong, K. P., Meng, K

Creator:: Shi, Xuhua, Kirby, Eric, Lu, Haijian, Robinson, Ruth, Furlong, Kevin P., and Wang, Erchie
Abstract:: Although geodetic measurements of interseismic deformation in interior Tibet suggest slow strain accumulation, active slip along the right-lateral Gyaring Co Fault is suggested to be between 8 and 21 mm/yr. Reliable geologic constraints on the slip rate along this fault are sparse. Here we document 12 ± 2 m of...
Full Text:: along the Gyaring Co fault, central Tibet Xuhua Shi1*, Eric Kirby2, Haijian Lu3, Ruth Robinson4

Creator:: Shi, Xuhua, Kirby, Eric, Furlong, Kevin P., Meng, Kai, Robinson, Ruth, and Wang, Erchie
Abstract:: Controversial end member models for the growth and evolution of the Tibetan Plateau demand quantitative constraints of the lithospheric rheology. Direct determinations of bulk crustal rheology, however, remain relatively sparse. Here we use the flexural rebound of lacustrine shorelines developed during the Lingtong highstand around Siling Co, in central Tibet,...
Resource Type:: Article

Creator:: Shi, Xuhua, Kirby, Eric, Lu, Haijian, Robinson, Ruth, Furlong, Kevin P., and Wang, Erchie
Abstract:: Although geodetic measurements of interseismic deformation in interior Tibet suggest slow strain accumulation, active slip along the right-lateral Gyaring Co Fault is suggested to be between 8 and 21 mm/yr. Reliable geologic constraints on the slip rate along this fault are sparse. Here we document 12 ± 2 m of...
Resource Type:: Article

Creator:: Shi, Xuhua, Furlong, Kevin P., Kirby, Eric, Meng, Kai, Marrero, Shasta, Gosse, John, Wang, Erchie, and Phillips, Fred
Abstract:: Subhorizontal lake shorelines allow a geodynamic test of the size and extent of a hypothesized paleolake in central Tibet, the East Qiangtang Lake (EQL), during the last interglacial period (marine isotope stage (MIS) 5e). Reconstructions based on relict lake deposits suggest that the EQL would have been ~400 m deep...
Resource Type:: Article
Full Text:: during the late Pleistocene Xuhua Shi1 , Kevin P. Furlong2 , Eric Kirby3 , Kai Meng4, Shasta Marrero5

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