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Velocity structure of the crust and uppermost mantle in the boundary area of the Tianshan Mountains and the Tarim Basin
A portable 3-component broadband digital seismic array was deployed across the Tianshan orogenic belt (TOB) to investigate the lithospheric structure. Based on receiver function analysis of the teleseismic P-wave data, a 2-D S-wave velocity profile of the boundary area of the TOB and the Tarim Basin was obtained at the depths of 0-80 km. Our results reveal a vertical and lateral inhomogeneity in the crust and uppermost mantle. Four velocity interfaces divide the crystalline crust into the upper, middle and lower crust. A low velocity zone is widely observed in the upper-middle crust. The depth of Moho varies between 42 and 52 km. At the north end of the profile the Moho dips northward with a vertical offset of 4-6 km, which implies a subduction front of the Tarim Basin into the TOB. The Moho generally appears as a velocity transitional zone except beneath two stations in the northern Tarim Basin, where the Moho is characterized by a typical velocity discontinuity. The fine velocity structure and the deep contact deformation of the crust and upper most mantle delineate the north-south lithospheric shortening and thickening in the boundary area of the TOB and the Tarim Basin, which would be helpful to constructing the geodynamical model of the intracontinental mountain-basin-coupling system.
作 者: MI Ning WANG Liangshu LI Hua Xu Mingjie Chen Yunping LI Cheng ZHANG Yong YU Dayong 作者單位: MI Ning,WANG Liangshu,LI Hua,Xu Mingjie,Chen Yunping,LI Cheng,YU Dayong(Department of Earth Sciences, Nanjing University, Nanjing 210093, China)ZHANG Yong(Seismological Bureau of Xinjiang Uygur Autonomous Region, Urumqi 830011, China)
刊 名: 科學(xué)通報(bào)(英文版) SCI 英文刊名: CHINESE SCIENCE BULLETIN 年,卷(期): 2005 50(3) 分類(lèi)號(hào): P5 關(guān)鍵詞: Tianshan orogenic belt receiver function low velocity zone mountain-basin-coupling system【Velocity structure of the crust and 】相關(guān)文章:
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