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

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  • 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 date: 2012-11-22

  Revised date: 2013-03-04

  Online published: 2013-06-10

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.

Cite this article

LU Xiao-yu,HUANG Zhi-long,WANG Bin,TANG Zhen-xing,HE Jun-ling,CUI Yang,TONG Ling . Research of Carboniferous-Permian Thermal History in Zhaoyuan Area of Songliao Basin[J]. Natural Gas Geoscience, 2013 , 24(3) : 548 -554 . DOI: 10.11764/j.issn.1672-1926.2013.03.548

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