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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2009-06
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Restoration of exhumation thickness and its significance in Sichuan Basin,China

DENG Bin,LIU Shu-gen,LIU Shun,LI Zhi-wu,ZHAO Jian-cheng State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China  
The inversion model of temperature-time depending on apatite fission track(AFT) can reconstruct 4-D dynamical uplift and exhumation history in sedimentary basins.The inversion of 93 AFT samples indicates that there has been a regional episodic cooling(110℃) since Late Cretaceous in Sichuan Basin.Sichuan Basin was quickly uplifted and exhumed during Late Cretaceous(~65 Ma B.P.) and Neogene(23 Ma B.P.~),but did slowly during Paleogene.The exhumation thickness in Sichuan Basin is generally more than 2.5 km since Late Cretaceous,while more than 1 km in Neogene.Comparing with 31 inversion and Easy-Ro(vitrinite reflectance) corrected data of erosion from Ro,this paper compiles the isopach map of the exhumation thickness during Neogene and since Late Cretaceous in Sichuan Basin.The total exhumation thickness has spread through NE-SW strike since Late Cretaceous,but E-W strike in Neogene.There has been a change of the tectonic background from Late Cretaceous to Neogene,resulting in multistage uplift and exhumation in Sichuan basin.There is a close relationship between the distribution of large to medium-sized oil and gas fields and the lower surface erosion thickness in Sichuan Basin.
【Fund】: 国家重点基础研究发展计划“973”项目(2005CB422106);; 中国石化海相前瞻性项目(PH08001)
【CateGory Index】: P618.13
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