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《地球科学学刊(英文版)》 2013-04
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Geothermal Evidence of the Mesozoic and Cenozoic Lithospheric Thinning in the Liaohe Depression

Yinhui Zuo* State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China; Research Center for Basin and Reservoir, China University of Petroleum, Beijing 102249, China; Research Institute of Exploration and Development, Zhongyuan Oilfield, SINOPEC, Puyang 457001, China Nansheng Qiu , Xiongqi Pang , Jian Chang State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China; Research Center for Basin and Reservoir, China University of Petroleum, Beijing 102249, China Qingqing Hao Institute of Mineral Resource Research, China Metallurgical Geology Bureau, Beijing 100025, China Xia Gao Research Institute of Exploration and Development, Zhongyuan Oilfield, SINOPEC, Puyang 457001, China  
The Liaohe (辽河) depression is an important part of the Bohai (渤海) Bay Basin, and the Bohai Bay Basin located in the center of lithospheric destruction and thinning in the eastern North China Craton. The North China lithospheric thinning activities have been verified from evidences of structural geology, petrology, geochemistry and geophysics, but there are still some controversies on their timing, mechanism and controlling factors. The sedimentary basin is a thin-bedded geologic unit with a limited distribution in the upper lithosphere, and its formation and evolution represent the shal-low response of the deep geodynamic process. Therefore, its thermal evolution is closely related to the deep dynamic conditions. In this article, the Mesozoic–Cenozoic thermal history of the Liaohe depression is reconstructed using the vitrinite reflectance and apatite fission track data. Meanwhile "thermal" lithospheric thicknesses in the Mesozoic and Cenozoic are calculated using the geothermic method on the basis of the above thermal history results. The results show that the Liaohe depression has undergone the Cretaceous and Paleogene heat flow peaks, 81 and 83 mW/m2, respectively, corresponding to two strong rift movements. Accordingly, the depression has experienced two different levels of thinning processes in the Cretaceous and the Paleogene since the Mesozoic, and the "thermal" lithospheric thicknesses were 60 and 50 km, respectively. This may reveal that the depression has experienced two large-scale destructions. The work may provide valuable geo-thermal evidence for initial revealing the time, process and stage of the lithospheric thinning in the Liaohe depression.
【Fund】: supported by the National Natural Science Foundation of China (Nos. 91114202 90914006);; the State Key Laboratory of Petroleum Resource and Prospecting (No.PRPJC2008-01);; the National Science Foundation Projectof CQ (No. CSTC2012jjb9007)
【CateGory Index】: P618.13
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