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《Earth Science(Journal of China University of Geosciences)》 2010-02
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Mesozoic Intra-Continental Progressive Deformation in Western Hunan-Hubei-Eastern Sichuan Provinces of China:Evidence from Apatite Fission Track and Balanced Cross-Section

MEI Lian-fu1,2,LIU Zhao-qian1,2,TANG Ji-guang3,SHEN Chuan-bo1,2,FAN Yuan-fang4 1.Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education,China University of Geosciences,Wuhan 430074,China 2.Faculty of Earth Resources,China University of Geosciences,Wuhan 430074,China 3.Yangtze University,Jingzhou 434023,China 4.Xi'an Petroleum University,Xi'an 710065,China  
The Mesozoic intra-continental evolution of about 400 km wide middle-upper Yangtze thrust belt from western Hunan-Hubei-eastern Sichuan provinces has been established with a time interval of 70 Ma (from 165 Ma to 95 Ma).Based on apatite fission track (AFT),time-temperature thermal history and balanced cross-section,we conclude that the deformation evolution is progressive from southeast (Jiangnan-Xuefeng intra-continental orogeny) to northwest (Huayingshan thrust belt),and younger and younger.The shortening of thick-skinned fault-fold zone in western Hunan Province-Hubei Province is less than that of thin-skinned fault-fold zone in east Sichuan Province.The shortening rate of the fault-fold zone in western Hunan Province-Hubei Province during Jurassic is obviously more than that of the southeast region of the fault-fold zone of eastern Sichuan Province during the early and middle periods of Early Crataceous.And the shortening rate of the southeast region of the fault-fold zone of eastern Sichuan Province during the early and middle periods of Early Crataceous is more than that of the northwest region of the fault-fold zone of eastern Sichuan Province during the late periods of Early Crataceous.The differences of the shortening rates in the different zones are controlled by the basement and the strength of the compressional deformation.These results indicate that Mesozoic intra-continental deformation in western Hunan Province-Hubei Province to eastern Sichuan Province is progressive with a large width and a long diachronous interval.Because of the different basement,basement involvement level and participation level of detachment layer,the differences of shorterning and shortening rates reflect the obvious differences of intra-continental deformation and its dynamics.The "driving engine" of Mesozoic intra-continental progressive deformation is speculated to be in Taoyuan-Huaihua area,if the Jiangnan-Xuefeng uplift is in place or parautochthon.The Taoyuan-Huaihua area is also where the Jiangnan-Xuefeng Mesozoic intra-continental orogenesis began and expanded southward and northward with a flower-structure geometry.
【Fund】: 中国石化海相前瞻性研究项目(Nos.YPH08 YPH08002);; 中国地质大学构造与油气资源教育部重点实验室开放研究基金项目(Nos.TPR-2009-01 TPR-2009-06 TPR-2009-26)
【CateGory Index】: P542
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