中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Modeling hydrocarbon accumulation based on gas origin and source rock distribution in Paleozoic strata of the Ordos Basin, China

文献类型:期刊论文

作者Liu, Dan2,3; Li, Jian1; Liu, Jia-qi2,3; Zhang, Lin4
刊名INTERNATIONAL JOURNAL OF COAL GEOLOGY
出版日期2020-05-15
卷号225页码:14
关键词Ordos Basin Paleozoic Natural gas Carbon isotope Coal-type gas Source rock
ISSN号0166-5162
DOI10.1016/j.coal.2020.103486
英文摘要Paleozoic gases in the Ordos Basin, China, are produced from upper Paleozoic tight sandstones, Ordovician weathered-crust, and 'pre-salt' (beneath gypsum deposits) dolomite reservoirs. Their origins have been debated, particularly as to whether Carboniferous-Permian (C-P) or Ordovician source rocks contributed more gas to the lower Paleozoic gas reservoirs. The expanded exploration of lower Paleozoic gas to the eastern, western, northern, and southern regions of the basin has re-initiated the debates. In this study, geochemical characteristics of gas samples from newly drilled wells in different regions of Ordos Basin in combination with the source rock evaluation were used to determine the gas origin. The carbon and hydrogen isotope of alkane indicate that gas mixing occurred in both upper Paleozoic and Ordovician weathered-crust gases, and that TSR occurred in pre-salt gases. A modified delta C-13-1/C-n plot was suggested to be useful to determine the carbon isotopic patterns of gases generated from the different source rocks. The light hydrocarbon characteristic shows that oil-type gas mainly distributes in the eastern basin. A study of source-rock distributions also indicates that the most favorable Ordovician source rock is located in the eastern basin. Based on the distribution of C-P coal measures, limestones and lower Paleozoic carbonate source rock, a gas accumulation history was established. The results of this study provide applicable method for identifying gas origin in Ordos Basin. Moreover, the accumulation history proposed in this study is useful for further exploration of the lower Paleozoic gas in Ordos Basin.
WOS关键词THERMOCHEMICAL SULFATE REDUCTION ; EAST SICHUAN BASIN ; NATURAL-GAS ; GEOCHEMICAL CHARACTERISTICS ; LIGHT-HYDROCARBONS ; THERMOGENIC GAS ; GENETIC TYPES ; ALKANE GASES ; PETROLEUM ; METHANE
资助项目National Natural Science Foundation for Young Scientists of China[41702161] ; China Geological Survey Program[DD20160170] ; China Geological Survey Program[DD20160203] ; China Geological Survey Program[DD20190090]
WOS研究方向Energy & Fuels ; Geology
语种英语
WOS记录号WOS:000536905200003
出版者ELSEVIER
资助机构National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; National Natural Science Foundation for Young Scientists of China ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program ; China Geological Survey Program
源URL[http://ir.iggcas.ac.cn/handle/132A11/96674]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Li, Jian
作者单位1.PetroChina Res Inst Petr Explorat & Dev, 20 Xueyuan Rd, Beijing 100083, Peoples R China
2.Chinese Acad Sci, Inst Earth Sci, 19 Beitucheng Western Rd, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, 19 Beitucheng Western Rd, Beijing 100029, Peoples R China
4.China Geol Survey, Il & Gas Survey, 267 Beisihuan Zhonglu Rd, Beijing 100083, Peoples R China
推荐引用方式
GB/T 7714
Liu, Dan,Li, Jian,Liu, Jia-qi,et al. Modeling hydrocarbon accumulation based on gas origin and source rock distribution in Paleozoic strata of the Ordos Basin, China[J]. INTERNATIONAL JOURNAL OF COAL GEOLOGY,2020,225:14.
APA Liu, Dan,Li, Jian,Liu, Jia-qi,&Zhang, Lin.(2020).Modeling hydrocarbon accumulation based on gas origin and source rock distribution in Paleozoic strata of the Ordos Basin, China.INTERNATIONAL JOURNAL OF COAL GEOLOGY,225,14.
MLA Liu, Dan,et al."Modeling hydrocarbon accumulation based on gas origin and source rock distribution in Paleozoic strata of the Ordos Basin, China".INTERNATIONAL JOURNAL OF COAL GEOLOGY 225(2020):14.

入库方式: OAI收割

来源:地质与地球物理研究所

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