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《Geological Bulletin of China》 2017-06
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LA-ICP-MS zircon U-Pb age of dykes from central Tarim Basin and its geological significance

LI Hang;Lü Haitao;PU Renhai;Department of Geology, Northwest University;Sinopec Northwest Oilfield Branch;  
Seismic data obtained from the central Tarim Basin show that lots of diabase dykes are developed in Cambrian, Ordovician and Permian strata. Diabase dykes that invaded into Silurian and Ordovician strata were collected near the fault zone(Zhong 1 well,Zhong 16 well core). Using LA-ICP-MS determination technology, the authors determined U-Pb age and trace elements in zircon. Zircon U-Pb age shows that the diabase dykes were formed in the Early Permian period of 273~296Ma. Measured 700~930Ma(Late Proterozoic) and 396~544Ma(Paleozoic) show the tectonic-magmatic activity when basin was formed. 121.0±8.5Ma(Early Cretaceous) zircon indicates that the formation was related to hydrothermal activities in the same period.
【Fund】: 中国石化西北油田分公司勘探开发研究院协作项目《顺南1井区三维工区海西期断裂与火山活动机制研究》(编号:KY2013-S-033)
【CateGory Index】: P588;P597.3;P618.13
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