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Kinetic Parameters of Methane Generated from Source Rocks in the Kuqa Depression of Tarim Basin and Their Application
Authors:LI Xianqing  XIAO Xianming  MI Jingkui  TANG Yongchun  XIAO Zhongyao  LIU Dehan  SHEN Jiagui  YANG Yunfeng  WANG Yan  DONG Peng
Affiliation:[1]State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China [2]State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Beijing 100083, China [3]Research Center of Petroleum Energy and Environment, California Institute of Technology, 21910 Currier Rd, Walnut, CA 61769, USA [4]Research Institute of Exploration and Development, Tarim Oil Field Company, PetroChina, Korla, Xinjiang 841000, China
Abstract:In a thermal simulation experiment of gold tubes of closed-system,calculating with the KINETICS and GOR-ISOTOPE KINETICS software,kinetic parameters of gas generation and methane carbon isotopic fractionation from Triassic-Jurassic hydrocarbon source rocks in the Kuqa depression of Tarim Basin are obtained.The activation energies of methane generated from Jurassic coal,Jurassic mudstone and Triassic mudstone in the Kuqa Depression are 197-268 kJ/mol,180-260 kJ/mol and 214-289 kJ/mol,respectively,and their frequency factors are 5.265x10~(13)s~(-1),9.761x10n~(11)s~(-1) and 2.270x10~(14)s~(-1).This reflects their differences of hydrocarbon generation behaviors.The kinetic parameters of methane carbon isotopic fractionation are also different in Jurassic coal,Jurassic mudstone and Triassic mudstone,whose average activation energies are 228 kJ/mol,205 kJ/mol and 231 kJ/mol,respectively.Combined with the geological background,the origin of natural gas in the Yinan-2 gas pool is discussed,and an accumulation model of natural gas is thus established.The Yinan- 2 gas is primarily derived from Jurassic coal-bearing source rocks in the Yangxia Sag.Main gas accumulation time is 5-0 Ma and the corresponding Ro is in the range from 1.25%-1.95%.The loss rate of natural gas is 25%-30%.
Keywords:hydrocarbon source rock  methane generation  carbon isotopic fractionation  kinetics  Kuqa Depression  Tarim Basin
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