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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2005-02
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Lower Cretaceous sequence stratigraphy of northern Coqen basin, Central Tibet, China

LI Xiang-hui~1, ZENG Qing-gao~2, WU Ge~3, MAO Guo-zheng~2, WANG Bao-di~2(1.State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China; 2.Tibet Geological Survey, Lhasa 851400, China;3. Peroleum Institute of Southwest Bureau, SINOPEC, Chengdu 610081, China)  
Twenty-three depositional sequence units are recognized in the Lower Cretaceous Chuanba Formation, Duoba Formation, and Langshan Formation in the northern Coqen basin, central Tibet. Of them, eleven depositional sequence units with average time-range 1.8 Ma are included in the Chuanba Formation, Duoba Formation, and twelve units with average 2.1 Ma in the Langshan Formation. The TST is dominated by terrigenous sediments, and HST are characterized by carbonate rocks in the first two formations, for which a sedimentary thickness texture style of TST≥HST is mostly superposed in each depositional sequence. The TST is composed of upward-deepening open platform facies, and the HST of upward-shallowing reef and / or bioclastic shoal facies in the Langshan Formation. A sedimentary thickness texture style of HST≥TST is often displayed in the last formation. It is supposed that the pattern of depositional sequences with systems tracts could imply a change of active regional to stable tectonism during the Early Cretaceous in the basin. The paper proposes that the HST rimmed reefs of the Langshan Formation in Nerma are prosperous for oil-gas exploration.
【Fund】: 中国地质调查局(I45C004001;I45C004002);; 国家自然科学基金(40273014)联合资助项目
【CateGory Index】: P539.2
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