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《Geochimica》 2004-06
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The ending time of gas generation of the Upper Paleozoic source rocks in Ordos basin using hydrocarbon gen eration kinetics

MI Jing-kui 1 ,LI Xin-hu 2 ,LIU Xin-hua 1 ,YANG Meng-da 1 ,YANG Rong-feng 1 1.School of Civil Engineering,Hunan University of Science and Technology,Xiangtan411201,China;2.Department of Geology and Environme ntal Engineering,Xian University of Science and Technology,Xian710054,China Correspondence should be addressed to MI Jing-kui(E-mail:jkmi@petrochina.com.cn)Received March 12,2004;revised July 14,2004;accepted July 29,2004;published November,2004  
There have been many reports about th e Upper Paleozoic gas pool in Ordos basin,but it is not clear or controversial whether source rock s till generated gas or not in the process of basin uplifting and when gas gen eration ended.In this paper,the gas generation history of representative well l ocated in the different area of the basin was calculated according to the results of simulation experiment and using h ydrocarbon generation kinetics software.The results show that the gas conversion ratio of source rock is the highest an d is more than 70%in the southern area of the basin,and it decreases from sout h to north.A lot of gases generated during uplifting of the basin,the amou nt of generated gas varies with the VRo of s ource rocks and the scope of temperature decreasing.Generally,the amou nt of generated gas in the western area i s greater than that in the southern on e in process of uplifting.The gas gen-eration ended in Early Tertiary in th e basin except the Tianhuan depression,the ending time of gas generation in the eastern area is earlier than that in t he western area.There is still littl e gas generation in Late Tertiary in t he Tianhuan depression.
【Fund】: 中国科学院知识创新工程重要方向项目(KZCX2-110);; 国家重大基础研究发展规划项目(2003CB214607)
【CateGory Index】: P618.13
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5 SUN Xu guang1, QIN Sheng fei2, LUO Jian2, JIN Kui li3(1. Department of Geology, Peking University, Beijing 100871, China; 2. Beijing Institute of Petroleum Exploration and Development, Beijing 100083, China;3.Beijing Graduate School, China University o;A study of activation energy of coal macerals[J];Geochimica;2001-06
6 XIONG Yong qiang, GENG An song, LIU Jin zhong, WANG Yun peng, LIU De han, JIA Rong fen, SHEN Jia gui(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China);Kinetic simulating experiment combined with GC-IRMS analysis: Application to identification of effective gas source rock[J];Geochimica;2002-01
7 ZHANG You sheng1, QIN Yong2, LIU Huan jie2, ZHU Yan ming2, JIANG Bo2, FAN Bing heng2(1. Faculty of Natural Resource and Information Technology, University of Petroleum, Beijing 102200, China; 2. College of Natural Resource and Environment Science, Chi;Investigation on the hydrocarbon regeneration from sedimentary organic mattersby pyrolytic simulation[J];Geochimica;2002-03
8 MI Jing kui1,2, XIAO Xian ming1, LIU De han1, SHEN Jia gui1(1. State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. Institute of Sedimentary Mineral and Resources,;Simulation for minimum trapping pressure of inclusions occurring in Upper Paleozoic sandstone reservoir of Ordos Basin using PVTsim[J];Geochimica;2002-04
9 SHUAI Yan-hua,ZOU Yan-rong,PENG Pi ng-an (State Key Laboratory of Organic Geochemistry,Guangzhou Institute of Ge ochemistry,Chinese Academy of Scie nces,Guangzhou510640,China);Kinetics modeling of stable carbon isotopes of coal-generated methane and its significance for gases accum ulation in the Kuqa Depression,Tarim Basin[J];Geochimica;2003-05
10 Wang Yigang Yu Xiaofeng Yang Yu Zhang Jing (Geology Exploration and Development Institute of Sichuan Petroleum Administration, Chengdu610051);APPLICATIONS OF FLUID INCLUSIONS IN THE STUDY OF PALEO GEOTEMPERATURE IN SICHUAN BASIN[J];;1998-03
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