The Geochemical Characteristics of The Carboniferous and Permian Source Rocks in the Western Henan,the southern North China Basin

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  • Henan Polytechnic University,Jiaozuo 454000,China

Received date: 2014-03-01

  Revised date: 2014-07-23

  Online published: 2015-01-10

Abstract

The purpose of the paper is to solve the problem about the hydrocarbon source rock recognition of Western Henan,the southern North China basin.Based on an extensive survey and observation of drilling cores,organic maceral identification,determination of residual  TOC,thermal analysis and vitrinite reflectance determination of hydrocarbon source rocks were used in the analysis of organic geochemistry feature of the Carboniferous and Permian source rocks in Western Henan.The study found that source rock,including carbonaceous mudstone,bioclastic limestone,coal,and dark mudstone,were influenced by the evolution of sedimentary environment.The best hydrocarbon source rocks originally should be the bioclastic limestone of Taiyuan Formation which deposited in the maximum transgression of the huge Transgressive-regressive cycles.However,the source rocks with type Ⅲ organic matter  and low hydrocarbon generation potential,mainly should be evaluated as poor source rocks or non-hydrocarbon source rock.The inversion phenomenon of low hydrocarbon generation potential was due to high thermal evolution,large amount of fracture development and the difference of CH4 adsorption capacity of different lithology.In Western Henan,the area where has excellent preservation conditions and affected by the regional thermal event slightly should be the favorable exploration area.

Cite this article

WU Wei,WANG Yu-han,CAO Gao-she,HUANG Xue-feng,LIU Wei-qing . The Geochemical Characteristics of The Carboniferous and Permian Source Rocks in the Western Henan,the southern North China Basin[J]. Natural Gas Geoscience, 2015 , 26(1) : 128 -136 . DOI: 10.11764/j.issn.1672-1926.2015.01.0128

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