Deep structure at northern margin of Tarim Basin
In this paper, a 2D velocity structure of the crust and the upper mantle of the northern margin of the Tarim Basin (TB) has been obtained by ray tracing and theoretical seismogram calculation under the condition of 2D lateral inhomogeneous medium using the data of seismic wide angle reflection/refra...
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Published in | Chinese science bulletin Vol. 53; no. 10; pp. 1544 - 1554 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
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SP Science in China Press
01.05.2008
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Abstract | In this paper, a 2D velocity structure of the crust and the upper mantle of the northern margin of the Tarim Basin (TB) has been obtained by ray tracing and theoretical seismogram calculation under the condition of 2D lateral inhomogeneous medium using the data of seismic wide angle reflection/refraction profile from Baicheng to Da Qaidam crossing the Kuqa Depression (KD) and Tabei Uplift (TU). And along the Baicheng to Da Qaidam profile, 4 of the 10 shot points are located in the northern margin of the TB. The results show that the character of the crust is uniform on the whole between the KD and TU, but the depth of the layers, thickness of the crust and the velocity obviously vary along the profile. Thereinto, the variation of the crust thickness mainly occurs in the middle and lower crust. The Moho has an uplifting trend near the Baicheng shot point in KD and Luntai shot point in TU, and the thickness of the crust reduces to 42 km and 47 km in these two areas, respectively. The transition zone between the KD and TU has a thickest crust, up to 52 km. In this transition zone, there are high velocity anoma- lies in the upper crust, and low velocity anomalies in the lower crust, these velocity anomalies zone is near vertical, and the sediment above them is thicker than the other areas. According to the velocity distributions, the profile can be divided into three sections: KD, TU and transition zone between them. Each section has a special velocity structural feature, the form of the crystalline basement and the relationship between the deep structure and the shallow one. The differences of velocity and tectonic between eastern and western profile in the northern margin of the Tarim Basin (NMTB) may suggest different speed and intensity of the subduction from the Tarim basin to the Tianshan orogenic belt (TOB). |
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AbstractList | In this paper, a 2D velocity structure of the crust and the upper mantle of the northern margin of the Tarim Basin (TB) has been obtained by ray tracing and theoretical seismogram calculation under the condition of 2D lateral inhomogeneous medium using the data of seismic wide angle reflection/refraction profile from Baicheng to Da Qaidam crossing the Kuqa Depression (KD) and Tabei Uplift (TU). And along the Baicheng to Da Qaidam profile, 4 of the 10 shot points are located in the northern margin of the TB. The results show that the character of the crust is uniform on the whole between the KD and TU, but the depth of the layers, thickness of the crust and the velocity obviously vary along the profile. Thereinto, the variation of the crust thickness mainly occurs in the middle and lower crust. The Moho has an uplifting trend near the Baicheng shot point in KD and Luntai shot point in TU, and the thickness of the crust reduces to 42 km and 47 km in these two areas, respectively. The transition zone between the KD and TU has a thickest crust, up to 52 km. In this transition zone, there are high velocity anoma- lies in the upper crust, and low velocity anomalies in the lower crust, these velocity anomalies zone is near vertical, and the sediment above them is thicker than the other areas. According to the velocity distributions, the profile can be divided into three sections: KD, TU and transition zone between them. Each section has a special velocity structural feature, the form of the crystalline basement and the relationship between the deep structure and the shallow one. The differences of velocity and tectonic between eastern and western profile in the northern margin of the Tarim Basin (NMTB) may suggest different speed and intensity of the subduction from the Tarim basin to the Tianshan orogenic belt (TOB). In this paper, a 2D velocity structure of the crust and the upper mantle of the northern margin of the Tarim Basin (TB) has been obtained by ray tracing and theoretical seismogram calculation under the condition of 2D lateral inhomogeneous medium using the data of seismic wide angle reflection/refraction profile from Baicheng to Da Qaidam crossing the Kuqa Depression (KD) and Tabei Uplift (TU). And along the Baicheng to Da Qaidam profile, 4 of the 10 shot points are located in the northern margin of the TB. The results show that the character of the crust is uniform on the whole between the KD and TU, but the depth of the layers, thickness of the crust and the velocity obviously vary along the profile. Thereinto, the variation of the crust thickness mainly occurs in the middle and lower crust. The Moho has an uplifting trend near the Baicheng shot point in KD and Luntai shot point in TU, and the thickness of the crust reduces to 42 km and 47 km in these two areas, respectively. The transition zone between the KD and TU has a thickest crust, up to 52 km. In this transition zone, there are high velocity anomalies in the upper crust, and low velocity anomalies in the lower crust, these velocity anomalies zone is near vertical, and the sediment above them is thicker than the other areas. According to the velocity distributions, the profile can be divided into three sections: KD, TU and transition zone between them. Each section has a special velocity structural feature, the form of the crystalline basement and the relationship between the deep structure and the shallow one. The differences of velocity and tectonic between eastern and western profile in the northern margin of the Tarim Basin (NMTB) may suggest different speed and intensity of the subduction from the Tarim basin to the Tianshan orogenic belt (TOB). |
Author | ZHAO JunMeng CHENG HongGang PEI ShunPing LIU HongBing ZHANG JianShi LIU BaoFeng |
AuthorAffiliation | Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100029, China Graduate University of Chinese Academy of Sciences, Beiiinc1100049, China Langfang Division of the Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, Langfang 065007, China Center for GeophysicaJ ExpJoration, China Earthquake Administration, Zhengzhou 450000, China |
Author_xml | – sequence: 1 givenname: JunMeng surname: Zhao fullname: Zhao, JunMeng email: zjm@itpcas.ac.cn organization: Institute of Tibetan Plateau Research, Chinese Academy of Sciences – sequence: 2 givenname: HongGang surname: Cheng fullname: Cheng, HongGang organization: Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Graduate University of Chinese Academy of Sciences, Langfang Division of the Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation – sequence: 3 givenname: ShunPing surname: Pei fullname: Pei, ShunPing organization: Institute of Tibetan Plateau Research, Chinese Academy of Sciences – sequence: 4 givenname: HongBing surname: Liu fullname: Liu, HongBing organization: Institute of Tibetan Plateau Research, Chinese Academy of Sciences – sequence: 5 givenname: JianShi surname: Zhang fullname: Zhang, JianShi organization: Center for Geophysical Exploration, China Earthquake Administration – sequence: 6 givenname: BaoFeng surname: Liu fullname: Liu, BaoFeng organization: Center for Geophysical Exploration, China Earthquake Administration |
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Cites_doi | 10.1360/04zd0020 10.1360/04zd0030 10.1360/04zd0024 10.1360/04zd0027 10.1029/93JB01560 10.1360/03yd0009 10.1016/j.tecto.2003.07.001 10.1002/cjg2.997 10.1016/j.epsl.2005.11.003 10.1007/BF02879522 |
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Keywords | Tianshan Orogenic Belt seismic reflection/refraction velocity structure northern margin of the Tarim Basin geodynamics |
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Notes | 11-1785/N P5 northern margin of the Tarim Basin, seismic reflection/refraction, velocity structure, geodynamics, Tianshan Orogenic Belt |
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Wang – volume: 47 start-page: 1 issue: Suppl.II year: 2004 ident: 117_CR10 publication-title: Sci China Ser D-Earth Sci doi: 10.1360/04zd0020 contributor: fullname: Z. J. Jin – volume: 47 start-page: 114 issue: Suppl.II year: 2004 ident: 117_CR15 publication-title: Sci China Ser D-Earth Sci doi: 10.1360/04zd0030 contributor: fullname: L. B. Zeng |
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Snippet | In this paper, a 2D velocity structure of the crust and the upper mantle of the northern margin of the Tarim Basin (TB) has been obtained by ray tracing and... In this paper, a 2D velocity structure of the crust and the upper mantle of the northern margin of the Tarim Basin (TB) has been obtained by ray tracing and... |
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SubjectTerms | Chemistry/Food Science Earth Sciences Engineering Humanities and Social Sciences Life Sciences multidisciplinary Physics Science Science (multidisciplinary) 地球动力学 地震活动 塔里木盆地北部 天山造山运动 流速结构 |
Title | Deep structure at northern margin of Tarim Basin |
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