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Palaeogeothermal response and record of the effusing of Emeishan basalts in the Sichuan basin
Authors:Zhu  ChuanQing  Xu  Ming  Yuan  YuSong  Zhao  YongQing  Shan  JingNan  He  ZhiGuo  Tian  YunTao  Hu  ShengBiao
Affiliation:1 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 
2 The Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 
3 Exploration and Production Research Institute, SINOPEC, Beijing 100083, China; 
4 Exploration Department of South Company of Prospecting, SINOPEC, Chengdu 610041, China; 
|5 Exploration and Development Research Institute of SINOPEC Southwest Branch, Chengdu 610081, China
Abstract:Thermal history of the Sichuan basin is reconstructed based on vitrinite reflectance from boreholes in the basin using a paleo-heat flow method.The results show that the Sichuan basin experienced a relatively low heat flow period in the Early Paleozoic,and an elevated paleo-heat flow,ranging 60-80 mW/m2 with a maximum as high as 100 mW/m2 around 259 Ma,from the beginning of the Late Paleozoic to the end of the early Permian,and a decreased paleo-heat flow from the late Permian to the late Triassic,and then ...
Keywords:vitrinite reflectance  paleo-heat flow method  thermal history  Emeishan mantle plume  Sichuan basin  
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