收稿日期: 2008-10-28
修回日期: 2008-11-03
网络出版日期: 2008-12-10
Coal-formed Gas Plays a Significant Role in the Natural Gas Industry of China
Received date: 2008-10-28
Revised date: 2008-11-03
Online published: 2008-12-10
戴金星,杨春;胡国艺;倪云燕;陶小晚 . 煤成气是中国天然气工业的主角[J]. 天然气地球科学, 2008 , 19(06) : 733 -740 . DOI: 10.11764/j.issn.1672-1926.2008.06.733
The coal-formed gas plays a leading role in the natural gas industry of China, which is verified by the following facts. First, the proved reserves of coal-formed natural gas are 39 583.80×108m3 by the end of 2007, 66.60% of the total natural gas reserves of China. Second, the numbers of gas fields, whose reserves are more than 300×108m3, are 41 by 2007 (except Taiwan). The proved coal\|formed reserves of these giant gas fields are 35 926.74×108m3, 60.45% of the total reserves in China. Third, there are 5 giant gas production areas including Sichuan basin, Tarim basin, Ordos basin, Yingqiong basin and Chaidam basin in China. Four of these areas have the coal formed gas production taking 90%~100% in their respective total gas production. The coal formed gas production in Sichuan accounts for only 26.29% of its total production.
Key words： Coal-formed gas; China; Natural gas industry; Giant gas field; Significant role.
［1] 傅诚德.天然气科学研究促进了中国天然气工业的起飞［G］//戴金星,傅诚德,关德范.天然气地质研究新进展.北京: 石油工业出版社,1997:1-11.
［2］戴金星,秦胜飞,陶士振,等.中国天然气工业发展趋势和天然气地学理论重要进展［J］.天然气地球科学,2005,16(2): 127-142.
［3］Жабрев,И.Л.и др.,Генезне газа и лрогноз газоносюсти[J].Гелогия Нефти и Газа 1979.No.9.
［4］戴金星.加强天然气地学研究勘探更多大气田［J］.天然气地球科学,2003,14(1): 3-14.
［5］李国玉,金之钧.新编世界含油气盆地图集(下册)［M］.北京: 石油工业出版社,2005:526-527.
［6］戴金星,邹才能,陶士振,等.中国大气田形成条件和主控因素［J］.天然气地球科学,2007,18(4): 473-484.
［7］张水昌,朱光有.中国沉积盆地大中型气田分布与天然气成因［J］.中国科学:D辑,2007,37(增刊Ⅱ):1-11.
［8］冯子辉,刘伟.徐家围子断陷深层天然气的成因类型研究［J］.天然气工业,2006,26(6): 18-20.
［9］张居和,冯子辉,霍秋立,等.混源天然气源岩贡献定量测试轻烃指纹技术［J］.石油学报,2006,27(增刊): 71-75.
［10］Feng Zhiqiang.Volcanic rocks as prolific gas reservoir: A case study from the Qingshen gas field in the Songliao Basin,NE China[J].Marine and Petroleum Geology,2008,25(4-5): 416-432.
［11］杨玉峰,张秋,黄海平,等.松辽盆地徐家围子断陷无机成因天然气及其成藏模式［J］.地学前缘,2000,7(4): 523-533.
［12］侯启军,杨玉峰.松辽盆地无机成因天然气及勘探方向探讨［J］.天然气工业,2002,22(3): 5-10.
［13］Dai J,Xia X,Qin S,et al.Origins of partially reversed alkane δ13C values for biogenic gases in China[J].Organic Geochemistry,2004,35(4): 405-411.［14］Hosgormez H.Origin of the natural gas seep of Cirali (Chimera),Turkey: Site of the first Olympic fire[J].Journal of Asian Earth Sciences,2007,30(1): 131-141.［15］Galimov E.M.Isotope organic geochemistry[J].Organic Geochemistry,2006,37(10):1200-1262.
［16］戴金星.天然气碳氢同位素特征和各类天然气鉴别［J］.天然气地球科学,1993,4(2-3): 1-40.
［17］朱扬明,王积宝,郝芳,等.川东宣汉地区天然气地球化学特征及成因［J］.地质科学,2008,43(3): 518-532.
［18］Fang Hao.Evidence for multiple stages of oil cracking and thermochemical sulfate reduction in the Pugang gas field,Sichuan Basin,China[J].AAPG Bulletin,2008,92(5):611-637.
［19］赵喆,钟宁宁,李艳霞,等.生烃化学动力学在川东北普光气田的应用［J］.石油勘探与开发,2006,33(6): 682-686.
［20］马永生,蔡勋育,郭彤楼.四川盆地普光大型气田油气充注与富集成藏的主控因素［J］.科学通报,2007,52(增刊Ⅰ): 149-155.
［21］Ma Yongsheng,Zhang Shuichang,Guo Tonglou,et al.Petroleum geology of the Puguang sour gas field in Sichuan Basin,SW China[J].Marine and Petroleum Geology,2008,25: 357-370.
［22］张水昌,朱光有,陈建平,等.四川盆地川东北部飞仙关组高含硫化氢大型气田群气源探讨［J］.科学通报,2007,52(增刊Ⅰ): 86-94.
［23］戴金星.威远气田成藏期及气源［J］.石油实验地质,2003,25(5): 473-480.
［24］邹才能,陶士振.中国大气区和大气田的地质特征［J］.中国科学:D辑,2007,37(增刊Ⅱ): 12-28.
［25］戴金星,陈践发,钟宁宁,等.中国大气田及气源［M］.北京: 科学出版社,2003:73-93.
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