刘丹, 冯子齐, 刘洋, 彭威龙, 韩文学 . 鄂尔多斯盆地中东部下古生界奥陶系自生自储气地球化学特征[J]. 天然气地球科学, 2016 , 27(10) : 1892 -1903 . DOI: 10.11764/j.issn.1672-1926.2016.10.1892

[1]Dai Jinxing,Wu Wei,Fang Chenchen,et al.Exploration and development of large gas fields in China since 2000[J].Natural Gas Industry,2015,35(1):1-9.[戴金星,吴伟,房忱琛,等.2000年以来中国大气田勘探开发特征[J].天然气工业,2015,35(1):1-9.][JP]
[2]Dai J,Li J,Luo X,et al.Stable carbon isotope compositions and source rock geochemistry of the giant gas accumulations in the Ordos Basin,China[J].Organic Geochemistry,2005,36:1617-1635.
[3]Xia Xinyu,Zhao lin,Li Jianfeng,et al.Geochemical characteristics and source rocks of Ordovician gas reservoirs,Changqing Gasfield[J].Chinese Science Bulletin,1999,44(10):1116-1119.[夏新宇,赵林,李剑锋,等.长庆气田天然气地球化学特征及奥陶系气藏成因[J].科学通报,1999,44(10):1116-1119.][JP]
[4]Huang Difan,Xiong Chuanwu,Yang Junjie,et al.Identification of origin of central gas field of Ordos Basin[J].Chinese Science Bulletin,1996,41(17):1588-1592.[黄第藩,熊传武,杨俊杰,等.鄂尔多斯盆地中部大气田的气源判识[J].科学通报,1996,41(17):1588-1592.]
[5]Zhang C,Sun F,Liu R,et al.Bitumen and hydrocarbon generation potential of paleo-reservoirs in the Ordovician,south Ordos Basin[J].Petroleum Exploration and Development,2010,37(6):668-673.
[6]Liu Dehan,Fu Jinhua,Zheng Congbin,et al.Research on hydrocarbon generation of Ordovician marine carbonatite of the Ordos Basin and genesis of Changqing Gasfields[J].Acta Geologica Sinica,2004(4):542-550.[刘德汉,付金华,郑聪斌,等.鄂尔多斯盆地奥陶系海相碳酸盐岩生烃性能与中部长庆气田气源成因研究[J].地质学报,2004(4):542-550.]
[7]Liu Q,Chen M,Liu W,et al.Origin of natural gas from the Ordovician paleo-weathering crust and gas-filling model in Jingbian Gasfield,Ordos Basin,China[J].Journal of Asian Earth Sciences,2009,35:74-88.
[8]Wu Zheng,Yang Yuanchu,Wang Xinhong.An analysis of the original-coexisting bitumen in Lower Ordovician in Ordos Basin[J].Natural Gas Industry,1999,19(6):14-17.[吴征,杨元初,王新红.鄂尔多斯盆地下奥陶统原生—同层沥青分析[J].天然气工业,1999,19(6):14-17.]
[9]Chen Anding.Feature of mixed gas in central gasfield of Ordos Basin[J].Petroleum Exploration & Development,2002,29(2):33-38.[陈安定.论鄂尔多斯盆地中部气田混合气的实质[J].石油勘探与开发,2002,29(2):33-38.]
[10]Ma Chunsheng,Xu Huazheng,Gong Changhong,et al.Paleo-oil reservoir and Jingbian natural gasfield of Ordovician weathering crust in Ordos Basin[J].Natural Gas Geoscience,2011,22(2):280-286.[马春生,许化政,宫长红,等.鄂尔多斯盆地中央隆起带奥陶系风化壳古油藏与靖边大气田关系[J].天然气地球科学,2011,22(2):280-286.]
[11]Xianqing L,Guoyi h,Jian L.The characteristics and sources of natural gases Central Gas Field in the Ordos Basin[J].Chinese Journal of Geochemistry,2008,2(27):109-120.
[12]Zhao Jingzhou,Wang Daxing,Sun Liuyi,et al.,Origin of the Ordovician gas and its accumulation patterns in northwestern Ordos Basin[J].Oil &Gas Geology,2015,36:711-720.[赵靖舟,王大兴,孙六一,等.鄂尔多斯盆地西北部奥陶系气源及其成藏规律[J].石油与天然气地质,2015,36:711-720.]
[13]Yang Hua,Zhang Wenzheng,Zan Chuanli,et al.Geochemical characteristics of Ordovician subsalt gas reservoir and their significance for reunderstanding the gas source of Jingbian Gasfield,east Ordos Basin[J].Natural Gas Geoscience,2009,20(1):8-14.[杨华,张文正,昝川莉,等.鄂尔多斯盆地东部奥陶系盐下天然气地球化学特征及其对靖边气田气源再认识[J].天然气地球科学,2009,20(1):8-14.]
[14]Yang Hua,Bao Hongping.Characteristics of hydrocarbon accumulation in the Middle Ordovician assemblages and their significance for gas exploration in the Ordos Basin[J].Natural Gas Industry,2011,31(12):11-20.[杨华,包洪平.鄂尔多斯盆地奥陶系中组合成藏特征及勘探启示[J].天然气工业,2011,31(12):11-20.]
[15]Yang Hua,Fu Jinhua,Wei Xinshan,et al.Natural gas exploration domains in Ordovician marine carbonates,Ordos Basin[J].Acta Petrolei Sinica,2011,32(5):733-740.[杨华,付金华,魏新善,等.鄂尔多斯盆地奥陶系海相碳酸盐岩天然气勘探领域[J].石油学报,2011,32(5):733-740.]
[16]Cai C,Hu G,He H,et al.Geochemical characteristics and origin of natural gas and thermochemical sulphate reduction in Ordovician carbonates in the Ordos Basin,China[J].Journal of Petroleum Science and Engineering,2005,48:209-226.
[17]Dai Jinxing,Zou Caineng,Li Wei,et al.Large coal-derived gas fields in China and their sources[M].Beijing:Science Press,2014:416-420.[戴金星,邹才能,李伟,等.中国煤成大气田及气源[M].北京:科学出版社,2014:416-420.]
[18]Wei Caiyun,Wang Huitong,Wang Hui,et al.Study on chloroform bitumen “A” exacted from rock using acceleraataed solvent extraction instrument[J].Modern Science Instrument,2009,2(12):96-98.[魏彩云,王汇彤,王慧,等.快速溶剂抽提仪萃取岩石中氯仿沥青“A”方法探索[J].现代科学仪器,2009,2(12):96-98.]
[19]Yu Cong,Huang Shipeng,Gong Deyu,et al.Partial reversal cause of carbon and hydrogen isotope compositions of natural gas:A case study in Sulige Gasfield,Ordos Basin[J].Acta Petrolei Sinica,2013,34(S1):92-101.[于聪,黄士鹏,龚德瑜,等.天然气碳、氢同位素部分倒转成因——以苏里格气田为例[J].石油学报,2013,34(S1):92-101.]
[20]Xia Xinyu.Hydrocarbon Potential Evaluation of Carbonates and Source Rock Correlation of the Changqing Gasfield[M].Beijing:Petroleun Industry Press,2000:48-51.[夏新宇.碳酸盐岩生烃与长庆气田气源[M].北京:石油工业出版社,2000:48-51.]
[21]Jin Qiang,Huang Zhi,Li Weizhen,et al.Sedimentary models of Ordovician source rocks in Ordos Basin and their hydrocarbon generation potential[J].Acta Geologica Sinica,2013,87(3):393-402.[金强,黄志,李维振,等.鄂尔多斯盆地奥陶系烃源岩发育模式和天然气生成潜力[J].地质学报,2013,87(3):393-402.][JP]
[22]Wang Wanchun,Zheng Jianjing,Wang Xiaofeng,et al.Comparisons of geochemical characteristics of Ordovician Majiagou carbonate rocks between west and south and central and east regions of Ordos Basin[J].Natural Gas Geoscience,26(3):513-523.[王万春,郑建京,王晓锋,等.鄂尔多斯盆地西南部与中东部奥陶系马家沟组碳酸盐岩地球化学特征对比[J].天然气地球科学,2015,26(3):513-523.]
[23]Dai Jinxing.Identification of different kinds of natural gas[J].Science in China:Series B,1992,22(2):185-193.[戴金星.各类烷烃气的鉴别[J].中国科学:B辑,1992,22(2):185-193.][JP]
[24]Yang Hua,Bao Hongping,Ma Zhanrong.Reservoir-forming by lateral supply of hydrocarbon:A new understanding of the formation of Ordovician gas reservoirs under gypsolyte in the Ordos Basin[J].Natural Gas Industry,2014,34(4):19-26.[杨华,包洪平,马占荣.侧向供烃成藏——鄂尔多斯盆地奥陶系膏盐岩下天然气成藏新认识[J].天然气工业,2014,34(4):19-26.][JP]
[25]Mi Jingkui,Wang Xiaomei,Zhu Guangyou,et al.Origin determination of gas from Jingbian Gasfield in Ordos Basin collective through the geochemistry of gas from inclusions and source rock pyrolysis[J].Acta Petrologica Sinica,2012,28(3):859-869.[米敬奎,王晓梅,朱光有,等.利用包裹体中气体地球化学特征与源岩生气模拟实验探讨鄂尔多斯盆地靖边气田天然气来源[J].岩石学报,2012,28(3):859-869.]
[26]Tilley B,Muehlenbachs K.Isotope reversals and universal stages and trends of gas maturation in sealed,self-contained petroleum systems[J].Chemical Geology,2013,339:194-204.
[27]Xia X,Chen J,Braun R,et al.Isotopic reversals with respect to maturity trends due to mixing of primary and secondary products in source rocks[J].Chemical Geology,2013,339:205-212.[JP]
[28]Machel H G,Krouse H R,Sassen R.Products and distinguishing criteria of bacterial and thermochemical sulfate reduction[J].Applied Geochemistry,1995,10:373-389.
[29]Worden R H,Smalley P C,Oxtoby N H.The effects of thermochemical sulfate reduction upon formation water salinity and oxygen isotopes in carbonate gas reservoirs[J].Geochimica et Cosmochimica Acta,1996,60:3925-3931.
[30]Prinzhofer A A,Huc A Y.Genetic and post-genetic molecular and isotopic fractionations in natural gases[J].Chemical Geology,1995,126(3/4):281-290.
[31]Behar F,Kressmann S,Rudkiewicz J L,et al.Experimental simulation in a confined system and kinetic modeling of kerogen and oil cracking[J].Advances in Organic Geochemistry,1991,19:173-189.
[32]Zeng H,Li J,Huo Q.A review of alkane gas geochemistry in the Xujiaweizi fault-depression,Songliao Basin[J].Marine and Petroleum Geology,2013,43:284-296.
[33]Zumberge J,Ferworn K,Brown S.Isotopic reversal(‘rollover’)in shale gases produced from the Mississippian Barnett and Fayetteville formations[J].Marine and Petroleum Geology,2012,31:43-52.