Aki K,Christoffersson A,Husebye E S.1977.Determination of the three-dimensional seismic structure of the lithosphere.J.Geophys.Res.,82(2);277～296.
[3]
Beaumont C,Jamiesont R A,Nguyen M H,et al.2001.Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation.Nature,414:738～742.
[4]
Burg J P,Davy P,Martinod J.1994.Shortening of analogue models of the continental lithosphere:New hypothesis for the formation of the Tibetan plateau.Tectonics,13:475～483.
[5]
Chen W P,Molnar P.1990.Source parameters of earthquakes and intraplate deformation beneath the Shillong plateau and the northern indoburman ranges.J.Geophys.Res,95:12527～12552.
[6]
Vera Schulte Pelkum,Gaspar Monsalve,Anne Sheehan,et al.2005.Imaging the Indian subcontinent beneath the Himalaya.Nature,435(30):1222～1225.
[7]
Zeng Rongsheng,Sun Weiguo.1992.Seismicity and focal mechanism in Tibetan Plateau and its implications to lithospheric flow.Acta Seism Sinica,14 (Suppl.):534～563.
Burchfiel B C,Chen Z L,Hedges K V,Liu Y P,Liu L H,Royden C R,Xu J N.1992.The South Tibet Detachment System.Himalayan orogeny:Extension contemporaneous with and parallel to shortening in a collisional mountain belt.Geol.Soc.Am.Special Paper,269:1～41.
[11]
Wittlinger G,Tapponnier P,Poupinet G,et al.1998.Tomographic Evidence for Localized Lithospheric Shear Along the Altyn Tagh Fault.Science,282:74～76.
[12]
Xiao Xuchanng,Li Tingdong,Li Guangcen,et al.1998.Tectonic evolution of the lithoshhere of the Himalayas general principle.Beijing:Geological Publishing House (in Chinese).
[13]
Zhao Wenjin & the Group of INDEPTH.2001,The study of Himalaya and the Deep Structure in Yaluzangbu Suture.Beijing:Geological Publishing House (in Chinese).
