[1]Liao Qianjin,Huang Difan,Xu Yongchang.Studies on geochemical characters [JP]of immature and lowmature oils from terrestrial formation in China[M]//Annual Research Report of Biogeochemistry and Gas Geochemistry Laboratory1986.Lanzhou:Gansu Publishing House of Science and Technology,1987:3460.[廖前进,黄第藩,徐永昌.我国陆相地层中未成熟、低成熟油的地球化学特征[M].中国科学院兰州地质研究所生物、气体地球化学开放研究实验室研究年报—1986.兰州:甘肃科学技术出版社,1987:3460.]
[2]Huang Difan,Liao Qianjin,Xu Yongchang.Preliminary studies on the genesis of immature petroleum[M]//Annual Research Report of Biogeochemistry and Gas Geochemistry Laboratory1987.Lanzhou:Gansu Publishing House of Science and Technology,1988:119.[黄第藩,廖前进,徐永昌.未成熟石油成因的初步研究[M].中国科学院兰州地质研究所生物、气体地球化学开放研究实验室研究年报—1987.兰州:甘肃科学技术出版社,1988:119.]
[3][KG*4/5]Huang Difan,Zhang Dajiang,Wang Peirong,et al.Genetic Mechanism and Accumulation Condition of Immature Oil in China[M].Beijing:Petroleum Industry Press,2003:625658.[黄第藩,张大江,王培荣,等.中国未成熟石油成因机制和成藏条件[M].北京:石油工业出版社,2003:625658.]
[4][KG*4/5]Mackenzie A S,Li Renwei,Maxwell J R,et al.Molecular measurement of thermal maturation of Cretaceous shales from the Overthrust Belt,Wyoming,USA[M]//Bjory M.Advances in Organic Geochemistry 1981.New York:J.Wiley and Sons,1983:637649.
[5]Beaumont C,Boutilier R,Machenzie A S,et al.Isomerization and aromatization of hydrocarbons and the paleothermometry and burial history of Albert Foreland Basin[J].AAPG Bulletin,1985,69(4):546566.
[6]Marzi R,Rullktter J.Qualitative and quantitative evolution and kinetics of biological marker transformationLaboratory experiments and applications to the Michigan Basin[M]//Moldowan J M,Albrecht P,Philp R P. Biological Markers in Sediments and Petroleum.New Jersey:Prentice Hall,1992:1841.
[7]Serfort W K,Moldowan J M.Use of biological markers in petroleum exploration[M]//Johns R B.Methods in Geochemistry and Geophysics.Amsterdam:Elsevier,1986,24:261290.[JP]
[8]Mackenzie A S,McKenzie D.Isomerization and aromatization of hydrocarbons in sedimentary basins formed by extension[J].Geology Magazine,1983,120:417470.
[9]Huang Difan,Li Jinchao,Zhang Dajiang,et al.Maturation sequence of Tertiary crude oils in the Qaidam Basin and its significance in petroleum resource assessment[J].Journal of Southeast Asian Earth Sciences,1991,5(14):359366.
[10]Wang Tieguan,Zhong Ningning,Hou Dujie,et al.Information and Occurrence of Lower Petroleum[M].Beijing:Petroleum Industry Press,1995:128151.[王铁冠,钟宁宁,侯读杰,等.低成熟油气形成机理与分布[M].北京:石油工业出版社,1995:128151.]
[11]Shi Yang,Bao Jianping,Zhu Cuishan,et al.Comparative study on geochemistry between crude oils from Qigequan and Xianshuiquan Oilfields in western Qaidam Basin[J].Natural Gas Geoscience,2010,21(1):132138.[施洋,包建平,朱翠山,等.柴达木盆地西部七个泉与咸水泉油田原油地球化学特征对比研究[J].天然气地球科学,2010,21(1):132138.]
[12][KG*4/5]Grantham P J.Sterane isomerization and moretane/hopane ratios in crude oils derived from Tertiary source rocks[J].Organic Geochemistry,1986,9(6):293304.
[13]Wingert W S.GCMS analysis of diamondoid hydrocarbon in smackover petroleum[J].Fuel,1992,71(1):3743.
[14]Williams J A,Bjory M,Dolcater D L,et al.Biodegradation in South Texas Eocene oil—Effects on aromatic and biomarkers[J].Organic Geochemistry,1986,10(13):451461.
[15]Chen J H,Fu J M,Sheng G Y,et al.Diamondoid hydrocarbon rations:Novel maturity indices for highly mature crude oil[J].Organic Geochemistry,1996,25(3/4):179190.
[16]Li Jinggui,Cui Mingzhou,Zhang Qian.A discussion about diamantane ratios as maturity indicators of Lower Paleozoic carbonate source rocks at high and over mature stages[J].Petroleum Exploration & Development,1998,25(2):8385.[李景贵,崔明中,张谦.双金刚烷指标作为下古生界高、过成熟阶段碳酸盐岩成熟度衡量标尺的讨论[J].石油勘探与开发,1998,25(2):8385.]
[17][KG*4/5]Guo Xiaowen,He Sheng,Cheng Honghan.Discussion and application of the maturity indicators of methyl double diamantane hydrocarbons[J].Geological Science and Technology Information,2007,26(1):7176.[郭小文,何生,陈红汉.甲基双金刚烷成熟度指标讨论与应用[J].地质科技情报,2007,26(1):7176.]
[18]Fang Chenchen,Wu Wei,Liu Dan,et al.Evolution characteristics and application of diamamondoids in coal measures[J].Natural Gas Geoscience,2015,26(1):110117.[房忱琛,吴伟,刘丹,等.煤系中金刚烷类化合物演化特征及应用[J].天然气地球科学,2015,26(1):110117.]
[19]Dahl J E,Moldowan J M,Peters K E,et al.Diamondoid hydrocarbons as indicators of natural oil cracking[J].Nature,1999,399(6):5457.
[20]Wei Z B,Moldowan J M,Zhang S C,et al.Diamondoid hydrocarbons as molecular proxy for thermal maturity and oil cracking:Geochemical models from hydrous pyrolysis[J].Organic Geochemistry,2007,38(2):227249.
[21]Zhang Shuichang,Zhao Wenzhi,Wang Feiyu,et al.Paleozoic oil cracking gas accumulation history from eastern part of the Tarim Basin[J].Natural Gas Geoscience,2004,15(5):441450.[张水昌,赵文智,王飞宇,等.塔里木盆地东部地区古生界原油裂解气成藏历史分析[J].天然气地球科学,2004,15(5):441450.]
[22]Zhang S C,Huang H P,Xiao Z Y,et al.Geochemistry of Palaeozoic marine petroleum from the Tarim Basin,NW China.Part 2:Maturity assessment[J].Organic Geochemistry,2005,36(8):12151225.
[23]Zhang S C,Su J,Wang X M,et al.Geochemistry of Palaeozoic marine petroleum from the Tarim Basin,NW China.Part 3:Thermal cracking of liquid hydrocarbons and gas washing as the major mechanism for deep gas condensate accumulations[J].Organic Geochemistry,2011,42(11):13941410.
[24][KG*4/5]Fu Ning,Li Youchuan.Diamondoid hydrocarbon ratios as indicators of maturity in natural gas[J].Acta Sedimentologica Sinca,2001,19(1):145149.[付宁,李有川.估算天然气成熟度的新指标—金刚烷指标[J].沉积学报,2001,19(1):145149.]
[25][KG*4/5]Li Sumei,Pang Xiongqi,Yang Haijun,et al.Geochemical characteristics and implication of high thermal maturity oils in TazhongⅠfaulted slope break zone[J].Oil & Gas Geology,2001,29(2):210216.[李素梅,庞雄奇,杨海军,等.塔中Ⅰ号坡折带高熟油气地球化学特征及其意义[J].石油与天然气地质,2001,29(2):210216.]
[26]Ma Anlai,Jin Zhijun,Zhu Cuishan,et al.Quantitative analysis on absolute concentration of diamondoids in oils from Tahe Oilfield[J].Acta Petrolei Sinica,2009,30(2):214218.[马安来,金之钧,朱翠山,等.塔河油田原油中金刚烷化合物绝对定量分析[J].石油学报,2009,30(2):214218.]
[27]Bao Jianping,Liang Xingyu,Zhu Cuishan,et al.Diamondoid hydrocarbons and their geochemical significances in condensate from the Zhujiadun gas reservoir in the Yancheng Sag[J].Natural Gas Geoscience,2015,26(3):505512.[包建平,梁星宇,朱翠山,等.盐城凹陷朱家墩气藏凝析油中的金刚烷类及其意义[J].天然气地球科学,2015,26(3):505512.]
[28]Ma Anlai,Zhou Jin,Lv Xueyan,et al.Geochemical characteristics and origin of Paleozoic condensates and natural gas in Block B,Saudi Arabia,Rub Al Khali Basin[J].Natural Gas Geoscience,2014,25(6):889897.[马安来,周瑾,吕雪雁,等.鲁卜哈利盆地沙特B区块古生界油气地球化学特征及成因[J],天然气地球科学,2014,25(6):889897.]
[29]Hou Dujie,Zhao Zengying,Tang Youjun,et al.The geological and geochemical characteristics of oil cracked gas in Kekeya region,Tarim Basin[J].Natural Gas Geoscience,2004,15(2):137141.[侯读杰,赵增迎,唐友军,等.柯克亚地区原油裂解气的地质—地球化学特征[J].天然气地球科学,2004,15(2):137141.]
[30]He Wenxiang,Wang Peirong,Pan Xianhuang,et al.The study of maturity of crude oils in Yingqiong Basin[J].Natural Gas Geoscience,2004,15(4):387390.[何文祥,王培荣,潘贤庄,等.莺—琼盆地原油成熟度研究[J].天然气地球科学,2004,15(4):387390.]
[31]He Guoyuan,Tan Yanhu,Guan Ping,et al.Research on Tertiary oil source in the northwest Qaidam Basin[J].Natural Gas Geoscience,2008,19(4):509518.[何国源,谭彦虎,关平,等.柴达木盆地西部北区第三系油源研究[J].天然气地球科学,2008,19(4):509518.]
[32]Jiang Xiaoqing,Lv Zonglun,Sun Bainian,et al.Evaluation of hydrocarbon source rocks in Xiaoliangshan Sag,western Qaidam Basin[J].Natural Gas Geoscience,2009,20(3):405410.[江小青,吕宗伦,孙柏年,等.柴达木盆地西部小梁山凹陷烃源岩评价[J].天然气地球科学,2009,20(3):405410.]
[33]Liang Digang,Chen Jianping.Oilsource correlations for high and over matured marine source rocks in south China[J].Petroleum Exploration and Development,2005,32(2):814.[梁狄刚,陈建平.中国南方高、过成熟区海相油源对比问题[J].石油勘探与开发,2005,32(2):814.]
[34]Bao Jianping,Ma Anlai,Li Xianqing.Geochemistry on Immature and Lower Mature Oils in Hypersaline Lacustrine Basin[M].Beijing:Geological Publishing House,2006:94134[包建平,马安来,李贤庆.江汉盐湖盆地未低熟油地球化学研究[M].北京:地质出版社,2006:94134]
[35]Fu Suotang.Key controlling factors of oil and gas accumulation in the western Qaidam Basin and its implication for favorable exploration direction[J].Acta Sedimentologica Sinica,2010,28(2):373379.[付锁堂.柴达木盆地西部油气成藏主控因素与有利勘探方向[J].沉积学报,2010,28(2):373379.] |