塔里木盆地东部沉积及成藏特征研究
|
摘要
研究区位于塔里木盆地东部,隶属于塔里木板块,包括孔雀河斜坡、英吉苏凹陷、罗布泊凹陷、塔东低凸起以及塔南隆起和塔东南拗陷的北部,约占整个盆地面积的四分之一。
在1960年以前,塔东地区石油地质工作仅限于地面地质调查,所调查的区域包括库鲁克塔格和阿尔金两个地区。区内首次石油勘探工作完成于上世纪六十年代,共完钻6口探井,未获油气显示。自塔里木石油勘探指挥部成立至今,在塔东地区展开了新一轮的油气勘探,相继在多口探井获得油气发现,打开了塔东地区油气勘探的新局面。
塔东地区的沉积盖层系统包括震旦系、古生界、中生界和新生界,沉积厚度近万米。多期构造活动的改造,总体表现为早古生代拉张裂陷、晚古生代抬升剥蚀、中新生代稳定沉降。在沉积演化上表现为六个阶段:震旦纪—奥陶纪演化阶段、志留纪—泥盆纪演化阶段、石炭纪—早二叠世演化阶段、晚三叠世—中侏罗世演化阶段、白垩纪演化阶段和新生代演化阶段。沉积环境的变迁直接影响到沉积相带的展布,最终决定了生、储、盖层的时空分布。
在塔东地区已证实有两套主要的烃源岩层系:海相的寒武系-下奥陶统烃源岩和陆相的侏罗系烃源岩。寒武系-下奥陶统烃源岩具有厚度大、分布广、丰度高、热演化程度高的特点,区内油气主要来源于该套烃源岩;侏罗系烃源岩是一套煤系源岩,成熟度低,现今仅达到未成熟-低成熟阶段,局部成熟的烃源岩以产低熟的凝析油气为主。中上奥陶统可能是本区一套潜在的烃源层系。
塔东地区储层类型包括碎屑岩和碳酸盐岩两大类。下志留统、侏罗系和下白垩统的碎屑岩储层和震旦系、寒武系的碳酸盐岩储层是主要的储层段。其中,侏罗系和下白垩统内的储层条件较好。下白垩统红色泥岩段和侏罗系克孜勒努尔组内的泥岩段是塔东地区的区域盖层,其他泥岩盖层,以及泥质岩夹煤层和致密砂岩盖层都属局部盖层。在研究区内共划分出10套储盖组合,震旦系—古生界和中生界各5套,以中生界储盖组合较好。
总结出三种成藏模式:古生古储早期油气聚集模式、古生新储晚期油气聚集模式、新生新储与新生古储晚期油气聚集模式。优选出7个油气勘探的有利区带,包括5个古生界有利区带、2个中生界有利区带。
The study area, which belongs to Tarim plate according to structural division, is located in the east of Tarim basin,and consists of Kongquehe slope,Yingjisu depression,Luobupo depression,and the north area of Tadong lower uplift and south-eastern depression.This area is nearly 25 percent of Tarim basin.Only the geologic ground survey had been completed before 1960 , including Kuluketage area and Aerjin area. Six exploratory wells had been drilled during 1960s with finding nothing, and it is the first time to drill for oil exploration in this area. The newly oil exploration work has been performing from the founding of Tarim headquarters to now. Oil and gas accumulations have been found in several wells, which indicates that the new era of oil and gas exploration is coming.The depositional cover incloudes Sinian system, Palaeozoic group, Mesozoic group, and Cainozoic group. The depositional thickness of all is nearly 10000 metres. Much tectogenesis had occurred in the past. The representation of tectogenesis is different in every geologic epoch, pull-apart depression in early Palaeozoic, uplift-denude area in late Palaeozoic, stable subsidence depression in Mesozoic era and Cenozoic era. There are six sedimentary evolution stages, such as, Sinian-Ordovician stage, Silurian-Devonian stage, Carboniferous-early Dias stage, late Triassic-middle Jurassic stage, Cretaceous stage,and Cenozoic stage. The change of sedimentary environment directly affects the distribution of sedimentary facies which determines the special distribution of oil sources, reservoirs and covers.Two oil source sets have been discovered. One comes from marine set of Cmbrian-lower Ordovician.The other comes from continental set of Jurassic. The Cmbrian-lower Ordovician source rock provides the mainly oil resource in study area which is thick,wide-ranging,lush and high maturation. The maturity index of Jurassic source rock, which comes from coal-measure strata, is lower. The thermal evolution of Jurassic source rock is in low-immature stage now. Partial mature source rock's product is mainly condensate. Middle-upper Ordovician maybe a potential oil source rock set.Two reservoir types are detrital reservoir rock and carbonate reservoir rock.The major reservoir sets are the detrital reservoir rock in lower Silurian, Jurassic, lower Cretaceous, and carbonate reservoir rock in Sinian and Palaeozoic in study area,among them the lower Silurian and Jurassic reservoir is better.The regional covers of study area are red mudstone in lower Silurian and the mudstone in Kezilenuer group of Jurassic.The other mudstone, argillaceous rock parting coal, as well as tight sandstone are local covers.There are ten reservoir-cover assemblages in study area,five in Sinian- Palaeozoic,the rest in Mesozoic whose assemblage is better.Three accmulation models have been summarized.The early accmulation model is Paleozoic source - Paleozoic reservoir. The late accmulation model is Paleozoic source -Mesozoic reservoir. The late accmulation model is Mesozoic source - Mesozoic reservoir or Paleozoic reservoir. There are seven favourable tectonic belts selected for exploration target in study area, five in Palaeozoic, the rest in Mesozoic .
在1960年以前,塔东地区石油地质工作仅限于地面地质调查,所调查的区域包括库鲁克塔格和阿尔金两个地区。区内首次石油勘探工作完成于上世纪六十年代,共完钻6口探井,未获油气显示。自塔里木石油勘探指挥部成立至今,在塔东地区展开了新一轮的油气勘探,相继在多口探井获得油气发现,打开了塔东地区油气勘探的新局面。
塔东地区的沉积盖层系统包括震旦系、古生界、中生界和新生界,沉积厚度近万米。多期构造活动的改造,总体表现为早古生代拉张裂陷、晚古生代抬升剥蚀、中新生代稳定沉降。在沉积演化上表现为六个阶段:震旦纪—奥陶纪演化阶段、志留纪—泥盆纪演化阶段、石炭纪—早二叠世演化阶段、晚三叠世—中侏罗世演化阶段、白垩纪演化阶段和新生代演化阶段。沉积环境的变迁直接影响到沉积相带的展布,最终决定了生、储、盖层的时空分布。
在塔东地区已证实有两套主要的烃源岩层系:海相的寒武系-下奥陶统烃源岩和陆相的侏罗系烃源岩。寒武系-下奥陶统烃源岩具有厚度大、分布广、丰度高、热演化程度高的特点,区内油气主要来源于该套烃源岩;侏罗系烃源岩是一套煤系源岩,成熟度低,现今仅达到未成熟-低成熟阶段,局部成熟的烃源岩以产低熟的凝析油气为主。中上奥陶统可能是本区一套潜在的烃源层系。
塔东地区储层类型包括碎屑岩和碳酸盐岩两大类。下志留统、侏罗系和下白垩统的碎屑岩储层和震旦系、寒武系的碳酸盐岩储层是主要的储层段。其中,侏罗系和下白垩统内的储层条件较好。下白垩统红色泥岩段和侏罗系克孜勒努尔组内的泥岩段是塔东地区的区域盖层,其他泥岩盖层,以及泥质岩夹煤层和致密砂岩盖层都属局部盖层。在研究区内共划分出10套储盖组合,震旦系—古生界和中生界各5套,以中生界储盖组合较好。
总结出三种成藏模式:古生古储早期油气聚集模式、古生新储晚期油气聚集模式、新生新储与新生古储晚期油气聚集模式。优选出7个油气勘探的有利区带,包括5个古生界有利区带、2个中生界有利区带。
The study area, which belongs to Tarim plate according to structural division, is located in the east of Tarim basin,and consists of Kongquehe slope,Yingjisu depression,Luobupo depression,and the north area of Tadong lower uplift and south-eastern depression.This area is nearly 25 percent of Tarim basin.Only the geologic ground survey had been completed before 1960 , including Kuluketage area and Aerjin area. Six exploratory wells had been drilled during 1960s with finding nothing, and it is the first time to drill for oil exploration in this area. The newly oil exploration work has been performing from the founding of Tarim headquarters to now. Oil and gas accumulations have been found in several wells, which indicates that the new era of oil and gas exploration is coming.The depositional cover incloudes Sinian system, Palaeozoic group, Mesozoic group, and Cainozoic group. The depositional thickness of all is nearly 10000 metres. Much tectogenesis had occurred in the past. The representation of tectogenesis is different in every geologic epoch, pull-apart depression in early Palaeozoic, uplift-denude area in late Palaeozoic, stable subsidence depression in Mesozoic era and Cenozoic era. There are six sedimentary evolution stages, such as, Sinian-Ordovician stage, Silurian-Devonian stage, Carboniferous-early Dias stage, late Triassic-middle Jurassic stage, Cretaceous stage,and Cenozoic stage. The change of sedimentary environment directly affects the distribution of sedimentary facies which determines the special distribution of oil sources, reservoirs and covers.Two oil source sets have been discovered. One comes from marine set of Cmbrian-lower Ordovician.The other comes from continental set of Jurassic. The Cmbrian-lower Ordovician source rock provides the mainly oil resource in study area which is thick,wide-ranging,lush and high maturation. The maturity index of Jurassic source rock, which comes from coal-measure strata, is lower. The thermal evolution of Jurassic source rock is in low-immature stage now. Partial mature source rock's product is mainly condensate. Middle-upper Ordovician maybe a potential oil source rock set.Two reservoir types are detrital reservoir rock and carbonate reservoir rock.The major reservoir sets are the detrital reservoir rock in lower Silurian, Jurassic, lower Cretaceous, and carbonate reservoir rock in Sinian and Palaeozoic in study area,among them the lower Silurian and Jurassic reservoir is better.The regional covers of study area are red mudstone in lower Silurian and the mudstone in Kezilenuer group of Jurassic.The other mudstone, argillaceous rock parting coal, as well as tight sandstone are local covers.There are ten reservoir-cover assemblages in study area,five in Sinian- Palaeozoic,the rest in Mesozoic whose assemblage is better.Three accmulation models have been summarized.The early accmulation model is Paleozoic source - Paleozoic reservoir. The late accmulation model is Paleozoic source -Mesozoic reservoir. The late accmulation model is Mesozoic source - Mesozoic reservoir or Paleozoic reservoir. There are seven favourable tectonic belts selected for exploration target in study area, five in Palaeozoic, the rest in Mesozoic .
引文
[1] 王德发,邓宏文.1992.陆源碎屑沉积环境及沉积体系.中国地质大学(北京),13-58
[2] 冯增昭,王英华,刘焕杰,沙庆安,王德发.1994.中国沉积学.北京:石油工业出版社,427～480
[3] 冯增昭.1993.沉积岩石学(第二版).北京:石油工业出版社,74～261
[4] 周志毅,陈丕基.1990.塔里木生物地层和地质演化.北京:科学出版社,56～126
[5] 周志毅,赵治信等.2001.塔里木盆地各纪地层.北京:科学出版社,81～366
[6] 冯增昭,王英华,刘焕杰,沙庆安,王德发.中国沉积学.北京:石油工业出版社.1994,427～480
[7] 赵治信,雍天寿,贾承造.1997.塔里木盆地地层.北京:石油工业出版社,76～93
[8] 曾强,2000.塔东地区勘探目标选择与评价.塔里木石油分公司内部报告
[9] 胡剑风.2003.英吉苏地区2002年勘探目标选择与评价.塔里木石油分公司内部报告
[10] 张丽娟等.塔里木盆地英吉苏地区中生界沉积储层研究.2002年自研项目,2002。
[11] 桑洪等.英吉苏凹陷2002年勘探目标选择与评价.2002年自研项目.2002。
[12] 冉启贵,魏伟等.塔东地区天然气综合评价及有利区带目标优选评价.廊坊分院内部报告,2003
[13] 朱如凯.塔里木盆地塔中地区志留系柯坪塔格组沉积相与沉积模式.古地理学报.2005,7(2):197～206
[14] 朱筱敏,王贵文,谢庆宾.塔里木盆地志留系层序地层特征.古地理学报.2001,3(2):64～71
[15] 朱筱敏,王贵文,谢庆宾.2002.塔里木盆地志留系沉积体系及分布特征.石油大学学报(自然科学版),26(3):5～12
[16] W.E.盖洛韦,D.K.霍布德,1989,陆源碎屑沉积体系在石油、煤和铀勘探中的应用,石油工业出版社,35～40
[17] 何登发、赵文智,中国西北地区沉积盆地动力学演化与含油气系统旋回,北京:石油工业出版社,1999。
[18] 贾承造、魏国齐等,塔里木盆地构造特征与油气聚集,96—111—01—01成果报告,1998。
[19] 周东延、李洪辉,塔里木盆地地震解释,95—101—01—01—02成果报告,1994。
[20] 顾家裕,宁从前,贾进华.塔里木盆地碎屑岩优质储层特征及成因分析[J].地质评论.1998,44(1):83-89
[21] 朱筱敏.1995.塔里木盆地志留系与泥盆系碎屑潮坪沉积.沉积学及岩相古地理新进展.北京:石油工业出版社,166～169
[22] 顾家裕主编.塔里木盆地沉积层序特征及其演化.北京:石油工业出版社.1996,1～316
[23] 顾家裕等.沉积相与油气.北京:石油工业出版社.1994,1～310
[24] 侯会军,王伟华,朱筱敏.塔里木盆地塔中地区志留系沉积相模式探讨.沉积学报.1997,15(3):41～47
[25] 朱筱敏,杨俊生,张喜林.岩相古地理研究与油气勘探.古地理学报.2004,6(1):101～109
[26] 何登发、李德生.塔里木盆地构造演化与油气聚集.北京:地质出版社,1996。
[27] 姜常义等.塔里木盆地东北缘构造演化及其对侏罗系烃源岩的控制作用.96—111成果报告,1999。
[28] 贾承造、魏国齐等.塔里木盆地构造特征.95—111—01—01成果报告,1994。
[29] 张光亚、贾进华等.塔里木板块构造演化、盆地综合分析与目标评价.“九五”项目成果报告,2000。
[30] 马郡等.塔东北地区石油地质综合评价研究(及附图册).内部成果报告,2000。
[31] 滇黔桂石油地质科学研究所塔里木地质队,阿尔金断隆古生代地层沉积相及含油性研究报告,1991。
[32] 滇黔桂石油地质科学研究所塔北一队.塔里木盆地东北缘库鲁克塔格地区震旦至奥陶纪地层沉积相及含油性研究报告.1989。
[33] 姜常义,吴文奎,李良辰.南天山东段显生宙构造演化.北京:地质出版社。1-160,2001。
[34] 高振家.再论天山地区的前寒武纪地层.新疆地质,8(1),1990
[35] 郭召杰,张志城.罗布泊形成及演化的地质新说.高校地质学报,1995,1(2):82-87。
[37] 郭召杰,张志城.阿尔金盆地群构造类型与演化.地质论评,1998a,44(4):357-364。
[38] 刘训,吴绍祖,傅德荣,姚建新,丁孝忠,王永,1997,塔里木板块周缘的沉积-构造演化。乌鲁木齐:新疆科技卫生出版社。
[39] 李德伦,段吉业,梁贵香,单玄龙,程新民.英吉苏凹陷中—新生代背驮式前陆盆地构造特征及成因机制.世界地质,2001,20(3):242-248。
[40] 杨瑞财,高伟中,杨彩虹,杜岚,苏武.塔里木盆地英吉苏凹陷中生界油气勘探潜力. 新疆石油地质,2000,21(3):184-187。
[41] 邬长武,刘震.塔东北地区侏罗系烃源岩评价.新疆石油地质,2000,21(3):201-203。
[42] 朱英,1989,塔里木东缘的若干大地构造问题。地球物理学报,32(4):399-408。
[43] 张用夏,1982,塔里木盆地区域构造特征。地球物理学报,25(3):243-338。
[44] 郑多明,李曰俊,杨来顺,卢玉红,2003,罗布泊凹陷石油地质条件。新疆石油地质,24(2):121-123。
[45] 宋岩、王毅等,天然气运聚动力学与气藏形成,石油工业出版社,2002。
[46] 爱德华 A. 博蒙特,诺曼 H. 福斯特主编,刘德来等译,油气勘探圈闭.北京:石油工业出版社.2002.
[47] 程克明,王兆云,熊英.中国碳酸盐岩的生烃研究.海相油气地质.4(4):1-11.1999.
[48] 郭秋麟,米石云等.盆地模拟原理方法.北京:石油工业出版社.1998.
[49] 郝石生等.下古生界高过成熟烃源岩特征和评价.勘探家.1(1):1996.
[50] 何登发,赵文智,雷振宇等.中国叠合型盆地复合含油气系统的基本特征.2000.
[51] 何登发、李德生.沉积盆地动力学研究新进展.地学前缘.2:1995.
[52] 胡见义.海相石油天然气地质综论.海相油气地质.1996.
[53] 李德生.中国含油气盆地的构造类型.石油学报.1982.
[54] 李思田.沉积盆地的动力学分析.地学前缘.1995.
[55] 李泰明.石油地质过程定量研究概论.东营:石油大学出版社,1989
[56] 田世澄,张树林,袁国礼等.论成藏动力学系统的划分和类型.见:胡见义,赵[57]文智主编.中国含油气系统的应用与进展.北京:石油工业出版社.1997.
[58] 翟光明等.论油气分布的有序性.石油学报.2000.21(1):1-9.2000.
[59] 赵文智,窦立荣,宋岩.我国天然气地质研究与勘探的新进展.天然气工业.2000.22(1):6-13 2001.
[60] 周东延,李洪辉.油气运移动态富集概念及其在塔里木台盆区油气勘探中的应用.石油勘探与开发.27(1):2-6 2000.
[61] 周兴熙等.塔里木盆地天然气形成条件及分布规律.北京:石油工业出版社.1998.
[62] 周兴熙,李绍基等.塔里木盆地凝析气藏形成.石油勘探与开发.23(6):7-11.1996.
[63] 朱夏.我国陆相中新生界含油气盆地的大地构造特征及有关问题.见:中国大地构造问题论文集.北京:科学出版社 1965.
[64] 朱夏.关于我国陆相中新生界含油气盆地若干基本地质问题的初步设想.石油实验地 质专辑 1978.
[65] Basin Compartments and Seals. AAPG Memoir, 61: 55-68
[66] Allen P. A. & J. R.Allen. 1990, Basin Analysis-Principles & Applications. Blackwell Scientific Publications, 282-308.
[67] Carmalt, S. W.&B. ST. John. 1986. Giant oil and gas fields. In: M. T. Halbouty (ed): Furure petroleum provinces of the world. AAPG Memoir 40 OK: 11-53.
[68] Dickinson, W. R. and H. Yarborough 1976. Plate tectonics and hydrocarbon accumulation. AAPG, Education Conrse Note Series, No. 1.
[69] Zunsheng Jiao, and R. C. Surdam, 1994. Stratigraphic/diagenetic pressure seals in the muddy sandstone, Power River basin, Wyoming. In Ortoleva P. J. eds., Basin Compartments and seals: AAPG Memoir, 61: 297-312.
[70] Welte D H, Horsfield B, Baker D R. 1997. Petroleum and basin evaluation. Saladruck, Berlin: Springer Verlag.
[71] Wilkinson, M. W., D. Darby, et al. 1997. Secondary porosity generation during deep burial associated with overpressure Leak-off: Fulmar Formation, UKCS AAPG Bull., 81: 803-813.
[72] Surdam, S. J., Zun, et al. 1994. Thermal maturarion, diagenesis and abnormal pressures in Cretaceous shales of the Laramide Basins of Wyoming, in abstracts from AAPG Hedberg Research Conference, Abnormal Pressure in Hydrocarbon Enviromments.
[73] Surdam, R. C., Zunshengjiao, Martinsen R. S. 1994. The regional pressure region in Cretaceous sandstones and shales in the Power River Basin. IN Ortoleva P. J. eds., Basin Compartments and seals. AAPG Memoir 61: 213-233.
[74] Sibson, R. H. 1994. Crustal stress, faulting and fluid flow, in J. Parnell, ed., Geofluids: origin, migration and evolution of fluids in sedimentary basins, Geological Society of London, Special Publication, No 78, 69-84.
[75] Downey, M. W., 1984, Evaluating seals for hydrocarbons accumulation, AAPG Bull. V. 68, No. 11, p.1752-1763.
[76] Nicoll R S.1984, Conodont colour alteration, thermal maturation and the geothermal history of the Canning Basin, Westem Australia. Austral Pet. Explor., Assoc. J., Vol.24, No.1, P.243-258
[77] Ferguson, J., 1988, Inorganic sources of hydrocarbons--Fact or fiction? (Meeting report), Journal of Petroleum Geology, V.11, No. 1, p.113-114.
[78] McLimas R K. 1985, Migration and maturation of hydrocarbons---Evidence from fluid inclutions (abs.), Bull. Artier. Assoc. Pet. Geol., Vol.69, No.2, p, 286.
[79] Curtis, G D., 1983, Link between aluminum mobility and destruction of secondary porosity, AAFG Bull. V. 67, No.3, 380～393.
[80] Mattavelli, L., et al, 1983, Geochemistry and habitat of natural gases in Po basin, Northern Italy, AAPG Bull., V67, 2239～2254.
[81] Rochl, P. O., and P. W. Choquctte(eds.), 1985, Carbonate petroleum reservoirs (Casebooks in earlh science), Springer-Vcrlag, New York.
[82] Coleman, D. D., et al., 1981, Fractionation of carbon and hydrogen isotopes by methane-oxidizing bacteria: Geochimica et Cosmochlmica Acta, V. 45, 1033-1037.
[83] Magara, K., 1986, Geological models of petroleum entrapment, Elsevier Applied Science Publishers LTD.
[84] Magoon, L.B., W.G. Dow (eds), 1991, Petroleum system--from source rock to trap, AAPG memoir, 62.
[85] Schoell. M, 1983, Genetic characterization of natural gases, AAPG Bull., V. 67, p. 2225-2238.
[86] Majorowicz A. 1985, The paleogeothermal and present thermal regimes of the Alberta Basin and their significances for petroleum occurrences. Bull. Can. Pet. Geol. Vol.33, No.1, p.12-21.
[2] 冯增昭,王英华,刘焕杰,沙庆安,王德发.1994.中国沉积学.北京:石油工业出版社,427～480
[3] 冯增昭.1993.沉积岩石学(第二版).北京:石油工业出版社,74～261
[4] 周志毅,陈丕基.1990.塔里木生物地层和地质演化.北京:科学出版社,56～126
[5] 周志毅,赵治信等.2001.塔里木盆地各纪地层.北京:科学出版社,81～366
[6] 冯增昭,王英华,刘焕杰,沙庆安,王德发.中国沉积学.北京:石油工业出版社.1994,427～480
[7] 赵治信,雍天寿,贾承造.1997.塔里木盆地地层.北京:石油工业出版社,76～93
[8] 曾强,2000.塔东地区勘探目标选择与评价.塔里木石油分公司内部报告
[9] 胡剑风.2003.英吉苏地区2002年勘探目标选择与评价.塔里木石油分公司内部报告
[10] 张丽娟等.塔里木盆地英吉苏地区中生界沉积储层研究.2002年自研项目,2002。
[11] 桑洪等.英吉苏凹陷2002年勘探目标选择与评价.2002年自研项目.2002。
[12] 冉启贵,魏伟等.塔东地区天然气综合评价及有利区带目标优选评价.廊坊分院内部报告,2003
[13] 朱如凯.塔里木盆地塔中地区志留系柯坪塔格组沉积相与沉积模式.古地理学报.2005,7(2):197～206
[14] 朱筱敏,王贵文,谢庆宾.塔里木盆地志留系层序地层特征.古地理学报.2001,3(2):64～71
[15] 朱筱敏,王贵文,谢庆宾.2002.塔里木盆地志留系沉积体系及分布特征.石油大学学报(自然科学版),26(3):5～12
[16] W.E.盖洛韦,D.K.霍布德,1989,陆源碎屑沉积体系在石油、煤和铀勘探中的应用,石油工业出版社,35～40
[17] 何登发、赵文智,中国西北地区沉积盆地动力学演化与含油气系统旋回,北京:石油工业出版社,1999。
[18] 贾承造、魏国齐等,塔里木盆地构造特征与油气聚集,96—111—01—01成果报告,1998。
[19] 周东延、李洪辉,塔里木盆地地震解释,95—101—01—01—02成果报告,1994。
[20] 顾家裕,宁从前,贾进华.塔里木盆地碎屑岩优质储层特征及成因分析[J].地质评论.1998,44(1):83-89
[21] 朱筱敏.1995.塔里木盆地志留系与泥盆系碎屑潮坪沉积.沉积学及岩相古地理新进展.北京:石油工业出版社,166～169
[22] 顾家裕主编.塔里木盆地沉积层序特征及其演化.北京:石油工业出版社.1996,1～316
[23] 顾家裕等.沉积相与油气.北京:石油工业出版社.1994,1～310
[24] 侯会军,王伟华,朱筱敏.塔里木盆地塔中地区志留系沉积相模式探讨.沉积学报.1997,15(3):41～47
[25] 朱筱敏,杨俊生,张喜林.岩相古地理研究与油气勘探.古地理学报.2004,6(1):101～109
[26] 何登发、李德生.塔里木盆地构造演化与油气聚集.北京:地质出版社,1996。
[27] 姜常义等.塔里木盆地东北缘构造演化及其对侏罗系烃源岩的控制作用.96—111成果报告,1999。
[28] 贾承造、魏国齐等.塔里木盆地构造特征.95—111—01—01成果报告,1994。
[29] 张光亚、贾进华等.塔里木板块构造演化、盆地综合分析与目标评价.“九五”项目成果报告,2000。
[30] 马郡等.塔东北地区石油地质综合评价研究(及附图册).内部成果报告,2000。
[31] 滇黔桂石油地质科学研究所塔里木地质队,阿尔金断隆古生代地层沉积相及含油性研究报告,1991。
[32] 滇黔桂石油地质科学研究所塔北一队.塔里木盆地东北缘库鲁克塔格地区震旦至奥陶纪地层沉积相及含油性研究报告.1989。
[33] 姜常义,吴文奎,李良辰.南天山东段显生宙构造演化.北京:地质出版社。1-160,2001。
[34] 高振家.再论天山地区的前寒武纪地层.新疆地质,8(1),1990
[35] 郭召杰,张志城.罗布泊形成及演化的地质新说.高校地质学报,1995,1(2):82-87。
[37] 郭召杰,张志城.阿尔金盆地群构造类型与演化.地质论评,1998a,44(4):357-364。
[38] 刘训,吴绍祖,傅德荣,姚建新,丁孝忠,王永,1997,塔里木板块周缘的沉积-构造演化。乌鲁木齐:新疆科技卫生出版社。
[39] 李德伦,段吉业,梁贵香,单玄龙,程新民.英吉苏凹陷中—新生代背驮式前陆盆地构造特征及成因机制.世界地质,2001,20(3):242-248。
[40] 杨瑞财,高伟中,杨彩虹,杜岚,苏武.塔里木盆地英吉苏凹陷中生界油气勘探潜力. 新疆石油地质,2000,21(3):184-187。
[41] 邬长武,刘震.塔东北地区侏罗系烃源岩评价.新疆石油地质,2000,21(3):201-203。
[42] 朱英,1989,塔里木东缘的若干大地构造问题。地球物理学报,32(4):399-408。
[43] 张用夏,1982,塔里木盆地区域构造特征。地球物理学报,25(3):243-338。
[44] 郑多明,李曰俊,杨来顺,卢玉红,2003,罗布泊凹陷石油地质条件。新疆石油地质,24(2):121-123。
[45] 宋岩、王毅等,天然气运聚动力学与气藏形成,石油工业出版社,2002。
[46] 爱德华 A. 博蒙特,诺曼 H. 福斯特主编,刘德来等译,油气勘探圈闭.北京:石油工业出版社.2002.
[47] 程克明,王兆云,熊英.中国碳酸盐岩的生烃研究.海相油气地质.4(4):1-11.1999.
[48] 郭秋麟,米石云等.盆地模拟原理方法.北京:石油工业出版社.1998.
[49] 郝石生等.下古生界高过成熟烃源岩特征和评价.勘探家.1(1):1996.
[50] 何登发,赵文智,雷振宇等.中国叠合型盆地复合含油气系统的基本特征.2000.
[51] 何登发、李德生.沉积盆地动力学研究新进展.地学前缘.2:1995.
[52] 胡见义.海相石油天然气地质综论.海相油气地质.1996.
[53] 李德生.中国含油气盆地的构造类型.石油学报.1982.
[54] 李思田.沉积盆地的动力学分析.地学前缘.1995.
[55] 李泰明.石油地质过程定量研究概论.东营:石油大学出版社,1989
[56] 田世澄,张树林,袁国礼等.论成藏动力学系统的划分和类型.见:胡见义,赵[57]文智主编.中国含油气系统的应用与进展.北京:石油工业出版社.1997.
[58] 翟光明等.论油气分布的有序性.石油学报.2000.21(1):1-9.2000.
[59] 赵文智,窦立荣,宋岩.我国天然气地质研究与勘探的新进展.天然气工业.2000.22(1):6-13 2001.
[60] 周东延,李洪辉.油气运移动态富集概念及其在塔里木台盆区油气勘探中的应用.石油勘探与开发.27(1):2-6 2000.
[61] 周兴熙等.塔里木盆地天然气形成条件及分布规律.北京:石油工业出版社.1998.
[62] 周兴熙,李绍基等.塔里木盆地凝析气藏形成.石油勘探与开发.23(6):7-11.1996.
[63] 朱夏.我国陆相中新生界含油气盆地的大地构造特征及有关问题.见:中国大地构造问题论文集.北京:科学出版社 1965.
[64] 朱夏.关于我国陆相中新生界含油气盆地若干基本地质问题的初步设想.石油实验地 质专辑 1978.
[65] Basin Compartments and Seals. AAPG Memoir, 61: 55-68
[66] Allen P. A. & J. R.Allen. 1990, Basin Analysis-Principles & Applications. Blackwell Scientific Publications, 282-308.
[67] Carmalt, S. W.&B. ST. John. 1986. Giant oil and gas fields. In: M. T. Halbouty (ed): Furure petroleum provinces of the world. AAPG Memoir 40 OK: 11-53.
[68] Dickinson, W. R. and H. Yarborough 1976. Plate tectonics and hydrocarbon accumulation. AAPG, Education Conrse Note Series, No. 1.
[69] Zunsheng Jiao, and R. C. Surdam, 1994. Stratigraphic/diagenetic pressure seals in the muddy sandstone, Power River basin, Wyoming. In Ortoleva P. J. eds., Basin Compartments and seals: AAPG Memoir, 61: 297-312.
[70] Welte D H, Horsfield B, Baker D R. 1997. Petroleum and basin evaluation. Saladruck, Berlin: Springer Verlag.
[71] Wilkinson, M. W., D. Darby, et al. 1997. Secondary porosity generation during deep burial associated with overpressure Leak-off: Fulmar Formation, UKCS AAPG Bull., 81: 803-813.
[72] Surdam, S. J., Zun, et al. 1994. Thermal maturarion, diagenesis and abnormal pressures in Cretaceous shales of the Laramide Basins of Wyoming, in abstracts from AAPG Hedberg Research Conference, Abnormal Pressure in Hydrocarbon Enviromments.
[73] Surdam, R. C., Zunshengjiao, Martinsen R. S. 1994. The regional pressure region in Cretaceous sandstones and shales in the Power River Basin. IN Ortoleva P. J. eds., Basin Compartments and seals. AAPG Memoir 61: 213-233.
[74] Sibson, R. H. 1994. Crustal stress, faulting and fluid flow, in J. Parnell, ed., Geofluids: origin, migration and evolution of fluids in sedimentary basins, Geological Society of London, Special Publication, No 78, 69-84.
[75] Downey, M. W., 1984, Evaluating seals for hydrocarbons accumulation, AAPG Bull. V. 68, No. 11, p.1752-1763.
[76] Nicoll R S.1984, Conodont colour alteration, thermal maturation and the geothermal history of the Canning Basin, Westem Australia. Austral Pet. Explor., Assoc. J., Vol.24, No.1, P.243-258
[77] Ferguson, J., 1988, Inorganic sources of hydrocarbons--Fact or fiction? (Meeting report), Journal of Petroleum Geology, V.11, No. 1, p.113-114.
[78] McLimas R K. 1985, Migration and maturation of hydrocarbons---Evidence from fluid inclutions (abs.), Bull. Artier. Assoc. Pet. Geol., Vol.69, No.2, p, 286.
[79] Curtis, G D., 1983, Link between aluminum mobility and destruction of secondary porosity, AAFG Bull. V. 67, No.3, 380～393.
[80] Mattavelli, L., et al, 1983, Geochemistry and habitat of natural gases in Po basin, Northern Italy, AAPG Bull., V67, 2239～2254.
[81] Rochl, P. O., and P. W. Choquctte(eds.), 1985, Carbonate petroleum reservoirs (Casebooks in earlh science), Springer-Vcrlag, New York.
[82] Coleman, D. D., et al., 1981, Fractionation of carbon and hydrogen isotopes by methane-oxidizing bacteria: Geochimica et Cosmochlmica Acta, V. 45, 1033-1037.
[83] Magara, K., 1986, Geological models of petroleum entrapment, Elsevier Applied Science Publishers LTD.
[84] Magoon, L.B., W.G. Dow (eds), 1991, Petroleum system--from source rock to trap, AAPG memoir, 62.
[85] Schoell. M, 1983, Genetic characterization of natural gases, AAPG Bull., V. 67, p. 2225-2238.
[86] Majorowicz A. 1985, The paleogeothermal and present thermal regimes of the Alberta Basin and their significances for petroleum occurrences. Bull. Can. Pet. Geol. Vol.33, No.1, p.12-21.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |