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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 2000-03
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MESOZOIC TECTONIC-PETROGRAPHIC EVOLUTION AND OIL-GAS PERSPECTIVE IN QIANGTANG BASIN,TIBET

YANG Ri_hong, LI Cai, YANG De_ming, HE Zhong_hua, REN Yun_sheng, LIU Shen (Changchun University of Science and Technology, Changchun 130026, China)  
The evolution history of Qiangtang basin is recorded by the tectonic-petrographic assemblage zones. There was a foreland-basin sedimentation in north Qiangtang at T 1 and T 2 period, but an erosion environment in south Qiangtang at the same time. In T 3, the centre upwarp belt was an erosion area, the north Qiangtang was still foreland-basin sedimentation, meanwhile, south Qiangtong had been already evolved to be a marginal sea sedimentation. In fact, the primary basin began to sag in J 1 and formed a narrow sedimentary belt. Owing to the continnous downwarping during J 2 period, the tectonic pattern of “two-sag and one-upwarp” of the basin was established. Qiangtang basin was wilted, cutoff and moulded in the end of Jurassic as the latest stage of basin development. The tectonic-petrographic assemblage evidences show that the medial Jurassic Longweihu-Quemocuo sag of north Qiangtang belt and Dirangbicuo sag of south Qiangtang belt are the favorable oil-gas prospective targets.
【Fund】: 中国石油天然气总公司青藏油气勘探项目经理部项目!(QZ - 95 - 2 0 412 7)
【CateGory Index】: P618.13
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