[1]米敬奎, 张水昌, 陈建平,等.轮南地区寒武系原油的分布特征[J].科学通报,2007,52(增刊I):101-107.
[2]赵孟军,秦胜飞,潘文庆,等.塔北隆起轮西地区奥陶系潜山油藏油气来源分析[J]. 新疆石油地质,2008,29(4):478-481.
[3]李素梅, 庞雄奇, 杨海军,等.塔中隆起原油特征与成因类型分析[J]. 地球科学,2008,33(5): 635-642.
[4]段毅, 于文修, 郑朝阳,等. 塔里木盆地塔河油田原油与源岩对比研究[J]. 沉积学报, 2009,27(1):164-171.
[5]梁狄刚,张水昌,赵孟军,等.库车拗陷的油气成藏期[J].科学通报,2002,47(增刊):56-63.
[6]秦胜飞,潘文庆,韩剑发,等.库车坳陷油气相态分布的不均一性及其控制因素[J].石油勘探与开发,2005, 32(2):19-22.
[7]包建平, 朱翠山, 张秋茶,等.库车坳陷前缘隆起带上原油地球化学特征[J]. 石油天然气学报(江汉石油学院学报), 2007,29(4):40-44.
[8]秦胜飞, 戴金星.库车坳陷煤成油、气的分布及控制因素[J]. 天然气工业, 2006,26(3):16-19.
[9]李谦,王飞宇,孔凡志,等.库车坳陷恰克马克组烃源岩特征[J]. 石油天然气学报(江汉石油学院学报), 2007,29(6):38-41.
[10]Jiang C Q, Li M W, Osadetz K G, et al. Bakken/Madison petroleum systems in the Canadian Williston Basins. Part 2: molecular markers diagnostic of Bakken and Lodgepole source rocks[J]. Organic Geochemistry, 2001, 32: 1037-1054.
[11]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, 2008, 29(2): 210-216.
[12]朱扬明,傅家谟,盛国英,等. 塔北地区不同海相源岩原油的识别[J]. 石油勘探与开发,1997, 24(6): 27-31.
[13]朱扬明.塔里木盆地陆相原油的地球化学特征[J].沉积学报, 1997,15(2):26-30.
[14]Leythaeuser D, Schaefer R G, Cornford C, et al. Generation and migration of light hydrocarbon (C2-C7) in sedimentary basins[J]. Organic Geochemistry, 1979,10(4): 191-204.
[15]Pang X Q, Li M W, Li S M. et al. Geochemistry of petroleum systems in the Niuzhuang South Slope of the Bohai Bay Basin. Part 2: evidence to significant contribution of mature source rocks to “immature oils” in the Bamianhe field[J]. Organic Geochemistry, 2003, 34(7): 931-950.
[16]Hughes W B, Holba A G, Dzuo L I P. The ratios of dibenzothiophene to phenanthrenes and pristane to phytane as indicators of the depositional environment and lithology of petroleum source rocks[J]. Geochimica et Cosmochimica Acta, 1995, 59(17): 3581-3598.
[17]于炳松,樊太亮. 塔里木盆地寒武系-奥陶系泥质烃源岩发育的构造和沉积背景控制[J]. 现代地质, 2008, 22(4): 534-540.
[18]Moldowan J M, Fago F J, Carlson R M K. Rearranged hopanes in sediments and petroleum[J]. Geochemica et Cosmchimica Acta, 1991, 55(11): 3333-3353.
[19]Li M W, Bao J P, Lin R Z, et al. Revised models for hydrocarbon generation, migration and accumulation in Jurassic coal measures of the Turpan Basin, NW China[J]. Organic Geochemistry, 2001, 32: 1127-1151.
[20]Li M W, Lavern S, Robert M et al. Geochemical and petrological evidence for Tertiary terrestrial and Cretaceous marine potential petroleum source rocks in the western Kamchatka coastal margin, Russia[J]. Organic Geochemistry, 2006, 37: 304-320.
[21]Liang D G, Zhang S C, Chen J P. Organic geochemistry of oil and gas in the Kuqa depression of Tarim Basin, NW China[J]. Organic Geochemistry, 2003, 34 (7): 873-888.
[22]赵孟军, 张水昌. 17α(H)重排藿烷在塔里木盆地中的指相意义[J]. 石油勘探与开发, 2001, 28 (1) : 36-381.
[23]肖中尧,黄光辉,卢玉红,等.库车坳陷却勒1 井原油的重排藿烷系列及油源对比[J].石油勘探与开发,2004,31(2): 35-37.
[24]Lin R Z, Wang P R. PAH in fossil fuels and their geochemical significance[J]. Journal of Southeastern Asian Earth Science, 1988, 5: 257-262.
[25]Peters K E, Moldowan J M. The Biomarker Guide: Interpreting Molecular Fossils in Petroleum and Ancient Sediments[M]. Engelwood Cliffs, N J: Prentice Hall Inc, 1993: 25-65.
[26]Seifert W K, Moldowan J M. Applications of steranes, terpanes, and monoaromatics to maturation, migration, and source of crude oils[J]. Geochimica et Cosmochimica Acta, 1978, 42(1): 77-95.
[27]李素梅,姜振学,董月霞,等. 渤海湾盆地南堡凹陷原油成因类型及其分布规律[J]. 现代地质, 2008, 22(5): 817-823.
[28]Sieskind O, Joly G, Albrecht P. Simulation of the geochemical transformation of sterols: Superacid effects of clay minerals[J]. Geochimica et Cosmochimica Acta, 1979, 43(10): 1675-1679.
[29]赵孟军, 卢双舫, 李剑. 库车油气系统天然气地球化学特征及气源探讨[J]. 石油勘探与开发, 2002, 48 (6) : 64-71
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