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《Journal of Northwest University(Natural Science Edition)》 2009-03
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Cenozoic multi-stage deformation occurred in southwest Sichuan:Cause for the dismemberment of the proto-Sichuan Basin

WANG Er-qi1,2,YIN Ji-yun3 (1.Institute of Geology and Geophysics,Chinese Academy of Science,Beijing 100029,China;2.Department of Geology,Northwestern University,Xi′an 710069,China;3.Bureau of Geological Survey of Yunnan Province,Kunming 650051,China)  
Aim To reveal the process of dismemberment of the proto-Sichuan basin.Methods Deformation study on southwestern Sichuan.Results The structural study in the lower part of the Dadu River area in southwest Sichuan shows that the deformation in this region is characterized by a complex anticline with fold axis plunging to the east.The anticline is cored by the Proterozoic granite,overlain by the sedimentary sequence with age ranging from Sinian to Mesozoic,both marking the basement and sedimentary cover of the Yangtze block,respectively.The sedimentary cover rocks within the southwestern margin of the Sichuan basin were shortened along the northern flank of the anticline in N-S direction along a series of nose structures,whereas those within the Daliangshan region along the southern flank of the anticline were shortened in N-S direction along a series of linear syncline and anticline.Conclusion These structures can be defined as the products of interfering deformation,result from at least two events.One occurred in early Tertiary time,resulted in the separation between the Sichuan and Chuxiong basing,and as a consequence,the Sichuan basin was closed up;and another occurred in the late Cenozoic time,caused by the southeastward movement of the Tibetan plateau along the Xianshuhe-Xiaojiang strick-slip fault.
【Fund】: 中国科学院知识创新工程重要方向基金资助项目(KZCX2-YW-12);; 中石化总公司基金资助项目(50730800);; 国家基金委创新群体基金资助项目(40721003)
【CateGory Index】: P618.13
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