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《Chinese Journal of Geophysics》 2009-07
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Application of the (U-Th)/He thermochronometry to the tectono-thermal evolution of sedimentary basin——A case history of Well KQ1 in the Tarim Basin

QIU Nan-Sheng~(1,2),Peter Reiners~3,MEI Qing Hua~(1,2),JIANG Guang~(1,2),Nicolesco Stefan~3,TAO Cheng~41 State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Beijing 102249,China2 Basin and Reservoir Research Center,China University of Petroleum,Beijing 102249,China3 Department of Geology,University of Arizona,Tucson,USA4 Wuxi Research Institute of Petroleum Geology,SINOPEC,Wuxi 214151,China  
The (U-Th)/He thermochronometry of apatite or zircon has been used as a new technique to study the structural uplift and thermal history of sedimentary basins in recent years. Based on the tested apatite and zircon He ages data from drilling wells samples, an evolution model of apatite He ages with depth and/or temperature is built, which illustrates that the He closure temperature in apatite is about 85℃ in the Tarim basin.However,the zircon He ages reveals that these samples hadn't undergone its higher closure temperature.The thermal history since Ordovician in Well KQ1 has been modeled by using the He ages,AFT and R。 data.The modeling result shows that the thermal gradient was about 35.5℃/km in the end of Ordovician, and 33.3~34.5℃/km during the period of Silurian to Devonian,and it decreased to 27.6℃/km in.the end of Cretaceous.Therefore,the (U-Th)/He ages may provide a newly tool to rebuilt the thermal history of sedimentary basins,especially to the Low Paleozoic carbonate stratum in Tarim basin which is lack of normal thermal indicators.
【Fund】: 教育部重大项目(308005);; 国家“973”项目(2005CB422102);; 中石化股份有限公司重点项目资助.
【CateGory Index】: P618.13
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