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《Acta Geologica Sinica》 2006-08
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Mesozoic-Cenozoic Dynamics of Longmenshan Foreland Basin along the Eastern Margin of the Tibetan Plateau and Its Coupled Relationship with Continnent Collision

LI Yong 1), P. A. ALLEN 2), ZHOU Rongjun 3), A. L. DENSMORE 2), M. A. ELLIS 4) 1) National Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, Sichuan, 610059, China; 2) Institute of Geology, Department of Earth Sciences, ETH Zentrum, CH-8092 Zurich, Switzerland; 3) Institute of Earthquake Engineering,Seismological Bureau of Sichuan Province, Chengdu, Sichuan, 610041, China; 4) Center for Earthquake Research and Information,University of Memphis,3890 Central Avenue,Memphis, TN 38152, USA  
The Longmenshan foreland basin is one of typical foreland basins along the eastern margin of the Tibetan Plateau. The Late Triassic—Quaternary strata there, more than 10000 m thick, can be divided into six tectonic sequences by unconformities. Two depositional patterns of tectonic sequences have been distinguished: one is wedge-shaped and the other is tabular-shaped. The wedge-shaped tectonic sequences include Late Triassic, Late Jurassic and Late Cretaceous—Eogene tectonic sequences. The tabular-shaped tectonic sequences include Early to Middle Jurassic, Middle Cretaceous and Neogene to Quaternary tectonic sequences. The results indicate that the wedge-shaped tectonic sequences are sedimentary response of active thrusting and the tabular-shaped tectonic sequences are sedimentary response of strike slipping. Taking the Late Triassic the wedge-shaped foreland basin as an example of the typical wedge-shaped foreland basin, we used a one-dimensional analytical model to simulate the subsidence in the wedge-shaped foreland basin due to the emplacement of tectonic loads in the Longmenshan thrust belt on an elastic plate. Taking the Neogene to Quaternary tabular-shaped foreland basin as an example of the typical tabular-shaped foreland basin, we used a one-dimensional analytical model to simulate the subsidence and uplift in tabular-shaped foreland basin due to the erosional unloading in Longmenshan on an elastic plate. The results indicate that the migration rate of the orogenic wedge in the early wedge-shaped foreland basin history (c. Late Triassic) was rapid (maximum of 15 mm/a) compared to the slow migration rate (maximum of 6.7 mm/a) during the later stage of the wedge-shaped foreland basin evolution (c. Late Jurassic and Late Cretaceous—Eogene). We infer that the episodic thrusting activity of Longmenshan was driven by the accretion of the Cimmerian continents and the India—Eurasia collision. The Late Triassic wedge-shaped tectonic sequence was a sedimentary response to the Qiangtang—Eurasian collision, the Late Jurassic wedge-shaped tectonic sequence was a sedimentary response to the Lhasa—Eurasian collision, and the Late Cretaceous—Eogene wedge-shaped tectonic sequence was a sedimentary response to the Kohistan—Eurasian collision and the India—Eurasian collision.
【Fund】: 国家自然科学基金项目(编号49803013 40372084);; 高等学校博士学科点专项科研基金项目(编号20050616004);; 四川省重点学科建设项目(编号SZD0408)资助的成果
【CateGory Index】: P542.1
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9 YU Fusheng1,ZHANG Fangfeng2,YANG Changqing3,LI Xueliang1 and FENG Zicheng1(1.State Key Laboratory of Petroleum Resources and Processing,China University of Petroleum,Beijing 102249,China; 2.NO.4 Geological Team of Inner Mongolia Bureau of Geological Survey,Xilinhot 026000,Inner Mongolia,China; 3.Southwest Division Company,SINOPEC,Chengdu 610081,Sichuan,China);Physical Simulation and Major Deformation-Controlling Factors of Typical Structural Sections for Guankou Fault in the Front of Longmen Mountains[J];Geotectonica Et Metallogenia;2010-02
10 ZHU Chuan-qing1,XU Ming1,SHAN Jing-nan1,YUAN Yu-song3,ZHAO Yong-qing4,HU Sheng-biao1(1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China;3.Exploration and Production Research Insitute,SINPIEC,Beijing 100083 China;4.Exploration Department of South Company of Prospecting,Sinopec,Chengdu 610041,Sichuan,China);Quantifying the denudations of major tectonic events in Sichuan basin:Constrained by the paleothermal records[J];Geology in China;2009-06
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1 HUANG Fang~(1,2),LIU Qiong-Ying~(1,2),HE Li-Juan~(1*) 1 State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China 2 The Graduate University of Chinese Academy of Sciences,Beijing 100049,China;Tectono-thermal modeling of the Sichuan Basin since the Late Himalayan period[A];[C];2013
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