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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2009-03
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Basin-range coupling and sequence filling patterns of the Upper Triassic Xujiahe Formation in the Northeastern Sichuan analogous foreland basin,China

ZHAI Wen-liang1,ZHENG Rong-cai1,ZHU Ru-kai2,DAI Zhao-cheng1,GAO Hong-can11.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China;2.Key Laboratory of Oil and Gas Reservoir of CNPC,Beijing 100083,China  
According to the multifactorial analysis of boundary identification in high-resolution sequence and sedimentary sequences,the Upper Triassic Xujiahe Formation(T3x) in Northeast Sichuan are divided into two super-long-term and five long-term base-level cycle sequences.The sequence evolution and sequence filling patterns of the two grades can clearly reflect the coupling process between basin and range of the Upper Triassic Xujiahe Formation in the Northeastern Sichuan foreland basin.The characteristic is that in the lower basin-forming period of T3x2-T3x3,the Micangshan-Dabashan Mountains ridges were in the low amplitude tectonic uplift,the depression amplitude was low in the northeast regions,the material supply and the growth rate of the accommodation space were basically stable,the braided river delta-lake sedimentary system was dominant,and the deposit thickness in the sequence structure of the rising half-cycle and falling half-cycle was mainly in the same symmetry,reflecting the relative stability of strata and the balance of the coupling process between basin and mountain;In the upper basin-forming period of T3x4-T3x6,the Micangshan-Dabashan Mountains began the stage of strongly thrusting-napping and tectonic uplifting,the depression amplitude suddenly enlarged,the supply of clastic sediments suddenly increased and was more than the growth rate of the accommodation space,mainly developed the alluvial fan delta-braided river delta sedimentary system was dominant,the deposit thickness in the sequence structure of the rising half-cycle and falling half-cycle and filling patterns were mainly in the same symmetry inside the basin,but in the marginal basin,the non complete symmetry was dominant,in which the thickness of the rising half-cycle was more than that of the falling half-cycle,and in some areas,only the rising half-cycle have been reserved,reflecting the unbalance feature in the coupling process between basin and range.
【Fund】: 国家重大专项课题“大型油气及煤层气开发”(2008ZX05000-003-01)
【CateGory Index】: P618.13
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