天然气地球科学

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松辽盆地肇源地区石炭系—二叠系热演化史研究

逯晓喻,黄志龙,王斌,唐振兴,贺君玲,崔洋,佟玲   

  1. 1.中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249;
    2.中国石油吉林油田分公司,吉林 松原 138000;
    3.中国石油吉林油田分公司松原采气厂,吉林 松原 138000
  • 收稿日期:2012-11-22 修回日期:2013-03-04 出版日期:2013-06-10 发布日期:2013-06-10
  • 通讯作者: 逯晓喻luxiaoyu33@163.com. E-mail:luxiaoyu33@163.com.
  • 作者简介:逯晓喻(1985-),女,山西阳泉人,博士研究生,主要从事油藏地球化学和油气藏形成机理与分布规律研究.E-mail:luxiaoyu33@163.com.
  • 基金资助:

    全国油气资源战略选区调查与评价国家专项(编号:2009GYXQ12-02)资助.

Research of Carboniferous-Permian Thermal History in Zhaoyuan Area of Songliao Basin

LU Xiao-yu,HUANG Zhi-long,WANG Bin,TANG Zhen-xing,HE Jun-ling,CUI Yang,TONG Ling   

  1. 1.State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Beijing 102249,China;
    2.PetroChina Jilin Oil field Company,Songyuan 138000,China;
    3.Jilin Oilfield Gas Production Factory,Songyuan 138000,China
  • Received:2012-11-22 Revised:2013-03-04 Online:2013-06-10 Published:2013-06-10

摘要: 松辽盆地肇源地区镜质体反射率(RO)—深度(H)曲线在石炭系—二叠系顶部不整合面呈连续变化,表明石炭系—二叠系为后期深埋藏。通过Suggate标准图版确定研究区最大古地温梯度为石炭系—二叠系早白垩世抬升剥蚀前的古地温梯度。结合流体包裹体发育部位和均一温度可知石炭系—二叠系地层存在2期充注。研究表明,肇源地区石炭系—二叠系烃源岩后期深埋藏存在二次生烃,为二次生气有利区。

关键词: 石炭系—二叠系, 古地温, 镜质体反射率, 流体包裹体, 肇源地区

Abstract:

The curve of vitrinite reflectance (RO)-depth (H) is successive across the unconformity on top of Carboniferous-Permian strata in Zhaoyuan area,which means the Carboniferous-Permian buried deep during the later sedimentation.The maximal paleogeothermal gradient of the study area is the Carboniferous-Permian paleogeothermal gradient analyzed by R.P.Suggate standard plate.Based on the occurring positions and homogenization temperatures of fluid inclusions,there are twice hydrocarbon charges.The results show that the Carboniferous-Permian source rocks have a secondary hydrocarbon-generation after later deep burial,and Zhaoyuan area is the favorable area for secondary gas-generation.

Key words: Carboniferous-Permian, Paleogeotherm, Vitrinite reflectance, Fluid inclusion, Zhaoyuan area

中图分类号: 

  • TE122.1

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