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四川盆地中生代地热特征与前陆盆地构造、沉积作用
引用本文:朱传庆,饶松,徐明,胡圣标.四川盆地中生代地热特征与前陆盆地构造、沉积作用[J].地质科学,2011,46(1):194-202.
作者姓名:朱传庆  饶松  徐明  胡圣标
作者单位:中国科学院地质与地球物理研究所 北京 100029
基金项目:国家重点基础研究发展计划"973"项目,国家自然科学基金项目
摘    要:沉积盆地热体制与油气资源勘探有着密切的联系.基于石油钻井的Ro数据,采用古地温梯度法恢复了四川盆地钻井的最高古地温.结果显示,四川盆地西部、川东南和川东北的钻井,顶部的剥蚀量在3 700 m左右,盆地中部的剥蚀量约3 100 m.钻井古地温梯度在13.2~24.5℃/km之间,古热流在31.2~60.1 mW/m2之间...

关 键 词:镜质体反射率  古地温梯度  古热流  前陆盆地  四川盆地
收稿时间:2010-10-08
修稿时间:2010-10-22

The Mesozoic thermal regime of the Sichuan Basin and the relationship between it and the structural and sedimentary action of the foreland basin evolution
Zhu Chuanqing,Rao Song,Xu Ming,Hu Shengbiao.The Mesozoic thermal regime of the Sichuan Basin and the relationship between it and the structural and sedimentary action of the foreland basin evolution[J].Chinese Journal of Geology,2011,46(1):194-202.
Authors:Zhu Chuanqing  Rao Song  Xu Ming  Hu Shengbiao
Institution:Institute of Geology and Geophysics, Chinese Academy of Science,Beijing 100029
Abstract:Thermal history reconstruction of the sedimentary basin is significant to the study of oil and gas exploration.The paleo temperature profiles reconstructed based on the vitrinite reflectance data from boreholes in the Sichuan Basin using a paleo temperature gradient method.The results show that the erosion in the top of the boreholes was about 3700 m in the western,southeastern and northeastern Sichuan Basin,while was about 3100 m in the central basin.The paleo temperature gradient ranged 13.2~24.5 ℃/km,and the paleo heat flow ranged 31.2~60.1mW/m2.The minimum value occurred at the L1 borehole which located in the Longmenshan foreland basin,northwestern Sichuan Basin,while the maximal value occurred at the W28 borehole which located in the Weiyuan uplift,southern Sichuan Basin.As a result of the structural and sedimentary action of the foreland basin evolution in Mesozoic,the heat flow was low in the Longmenshan and Dabashan foreland basins.
Keywords:Vitrinite reflectance  Paleo temperature gradient  Paleo heat flow  Foreland basin  Sichuan Basin
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