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《Chinese Journal of Geophysics》 2014-06
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Tectonic and thermal history during the Mesozoic and Cenozoic era in Paizhouwan region,Jianghan Plain,Mid Yangtze Area

LI Tian-Yi;HE Zhi-Liang;HE Sheng;ZHOU Yan;SUN Dong-Sheng;WO Yu-Jin;YANG Xing-Ye;WANG Li;Laboratory of Structural and Sedimentological Reservoir Geology,Research Institute of Petroleum Exploration & Production,SINOPEC;Key Laboratory of Tectonics and Petroleum Resource of Ministry of Education,China University of Geosciences;Research Institute of Petroleum Exploration & Production,SINOPEC;  
In this paper,apatite and zircon fission track and(U-Th)/He dating,vitrinite reflectance analysis and basin modeling are carried out,for more clearly understanding the tectonic and thermal history during the Mesozoic and Cenozoic era of the Paizhouwan area,eastern Jianghan Basin.The analysis results show that the enormous tectonic uplift,erosion,and formation cooling event during the Mesozoic and Cenozoic began at the early Cretaceous(140-130 Ma);the intense tectonic uplift-cooling process mainly occurred during the early Cretaceous to the Late Cretaceous.While there may be some sediments of the Late Cretaceous-Paleogene period,the overall deposition thickness is relatively small.There should be large-scale sediments deposited during the Middle Jurassic or/and Upper Jurassic and even the early Cretaceous.The present-day remnant is thin,mainly due to the later successive erosion for which the total estimated denudation thickness is about 4300 m.The Mesozoic strata in the studied area reached the maximum paleotemperature in the Early Cretaceous,rather than at the Paleogene sedimentary final,the maximum temperature of the Upper Triassic is about 170~190℃.The thermal history results also show that the ancient heat flow is relatively stable during the Paleozoic era.The average value of the heat flow is about 53.64 mW ? m~(-2);the heat flow began to decrease at the early Jurassic,and the lowest is about 48.38 mW ? m~(-2) happened during the beginning of the early Cretaceous approximately.
【Fund】: 国家自然科学基金重点项目(40739904)、国家自然科学基金面上项目(41072093)、国家自然科学基金青年科学基金项目(41302117);; 国家“十一五”科技重大专项(2011ZX05005-002);; 中国石化勘探南方分公司合作项目(G0800-12-ZS-066)联合资助
【CateGory Index】: P618.13
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