Cowgill. 2007. Impact of riser reconstructions on estimation of secular variation in rates of strike-slip faulting: Revisiting the Cherchen River site along the Altyn Tagh Fault, NW China. Earth Planet Sci Lett, 254: 239-255
[38]
Guo J M, Lin A M, Sun G Q, et al. 2007. Surface ruptures associated with the 1937 M7.5 Tuosuo Lake and the 1963 M7.0 Alake Lake Earthquakes and the Paleoseismicity along the Tuosuo Lake Segment of the Kunlun Fault, Northern Tibet. Seism Soc Am Bull, 97: 474-496
[39]
England P, Molnar P. 1997. Active deformation of Asia: From kinematics to dynamics. Science, 278: 647-650
[40]
Harkins N, Kirby E. 2008. Fluvial terrace riser degradation and determination of slip rates on strike-slip faults: An example from the Kunlun fault, China. Geophys Res Lett, 35: L05406, doi: 10.1029/2007GL033073
[41]
Kidd W S F, Molnar P. 1988. Quaternary and active faulting observed on the 1985 Academia Sinica-Royal Society Geotraverse of Tibet. Philos Trans R Soc A-Math Phys Eng Sci, 327: 337-363
[42]
Kirby E, Harkins N, Wang E Q, et al, 2007. Slip rate gradients along the eastern Kunlun fault. Tectonics, 26: TC2010
[43]
Lin A M, Guo J M. 2008. Nonuniform slip rate and millennial recurrence interval of large earthquakes along the eastern segment of the Kunlun Fault, Northern Tibet. Bull Seismol Soc Amer, 98: 2866-2878
[44]
Peltzer G, Tapponnier P, Armijo R. 1989. Magnitude of Late Quaternary left-lateral displacements along the North Edge of Tibet. Science, 246: 1285-1289
[45]
Peltzer G, Crampé F, King G. 1999. Evidence of nonlinear elasticity of the crust from the Mw7.6 Manyi (Tibet) earthquake. Science, 286: 272-276
[46]
Royden L H, Burchfiel B C, King R W, et al. 1997. Surface deformation and lower crustal flow in Eastern Tibet. Science, 276: 788-790
[47]
Sieh K E, Jahns R H. 1984. Holocene activity of the San Andreas Fault at Wallace Creek, California. Geol Soc Am Bull, 95: 883-896
[48]
Tapponnier P, Peltzer G, Le Dain A Y, et al. 1982. Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine. Geology, 10: 611-616
[49]
Tapponnier P, Xu Z Q, Roger F, et al. 2001. Oblique stepwise rise and growth of the Tibet Plateau. Science, 294: 1671-1677
Avouac J P, Tapponnier P. 1993. Kinematic model of active deformation in central Asia. Geophys Res Lett, 20: 895-898
[55]
Van Der Woerd J, Tapponnier P, Ryerson F J, et al. 2002. Uniform postglacial slip-rate along the central 600 km of the Kunlun Fault (Tibet), from Al-26, Be-10, and C-14 dating of riser offsets, and climatic origin of the regional morphology. Geophys J Int, 148: 356-388
[56]
Wang X L, Lu Y C, Wintle A G. 2006. Recuperated OSL dating of fine-grained quartz in Chinese loess. Quat Geochronol, 1: 89-100
[57]
Wells D L, Coppersmith K J. 1994. New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull Seismol Soc Amer, 84: 974-1002
[58]
Xu X W, Yu G H, Klinger Y, et al. 2006. Reevaluation of surface rupture parameters and faulting segmentation of the 2001 Kunlunshan earthquake (Mw7.8), northern Tibetan Plateau, China. J Geophys Res, 111: B05316, doi: 10.1029/2004JB003488
[59]
Xu X W, Wen X, Yu G, et al. 2009. Co-seismic reverse- and oblique-slip surface faulting generated by the 2008 Mw7.9 Wenchuan earthquake, China. Geology, 37: 515-518
[60]
Zhang P Z, Shen Z K, Wang M, et al. 2004. Continuous deformation of the Tibetan Plateau from global positioning system data. Geology, 32: 809-812
[61]
Zhang P Z, Molnar P, Xu X W. 2007. Late Quaternary and present-day rates of slip along the Altyn Tagh Fault, northern margin of the Tibetan Plateau. Tectonics, 26: TC5010
