Bongor盆地Baobab地区潜山油气成藏期次

doi:10.7623/syxb201808003

石油学报 ›› 2018, Vol. 39 ›› Issue (8): 869-875.DOI: 10.7623/syxb201808003

Bongor盆地Baobab地区潜山油气成藏期次

文志刚¹, 李威^1,2,3, 窦立荣^1,4, 张光亚³, 程顶胜³, 杜业波³, 胡瑛³, 王利³

1. 长江大学资源与环境学院油气资源与勘探技术教育部重点实验室湖北武汉 430100;
2. 中海油研究总院有限责任公司北京 100028;
3. 中国石油勘探开发研究院北京 100083;
4. 中国石油天然气勘探开发公司北京 100034

收稿日期:2017-06-05 修回日期:2017-11-03 出版日期:2018-08-25 发布日期:2018-09-04
通讯作者: 文志刚,男,1965年7月生,1985年获江汉石油学院学士学位,1997年获中国地质大学(北京)博士学位,现为长江大学教授、博士生导师,主要从事有机地球化学及石油地质学研究。Email:wzg728@sina.com
作者简介:文志刚,男,1965年7月生,1985年获江汉石油学院学士学位,1997年获中国地质大学(北京)博士学位,现为长江大学教授、博士生导师,主要从事有机地球化学及石油地质学研究。Email:wzg728@sina.com
基金资助:
国家科技重大专项（2011ZX05029，2016ZX05029-005）、中国石油天然气股份有限公司科技专项（2013D-0902）资助。

Buried-hill hydrocarbon accumulation stage of Baobab area in Bongor Basin

Wen Zhigang¹, Li Wei^1,2,3, Dou Lirong^1,4, Zhang Guangya³, Cheng Dingsheng³, Du Yebo³, Hu Ying³, Wang Li³

1. College of Resources and Environment, Yangtze University;Key Laboratory of Exploration Technologies for Oil and Gas Resources of the Ministry of Education, Hubei Wuhan 430100, China;
2. CNOOC Research Institute Co. Ltd., Beijing 100028, China;
3. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China;
4. China National Oil and Gas Exploration and Development Corporation, Beijing 100034, China

Received:2017-06-05 Revised:2017-11-03 Online:2018-08-25 Published:2018-09-04

摘要/Abstract

摘要：

Baobab潜山油藏是乍得Bongor盆地北部斜坡的主力油藏。以Baobab C-2井潜山油藏为例，从烃源岩生排烃史、构造热演化史、流体包裹体中含油包裹体颗粒指数特征、显微荧光与测温技术等方面分析其油气成藏史。埋藏史的分析结果表明，Baobab地区Mimosa组+Prosopis组主力烃源岩在约90 Ma开始生烃，并于约80 Ma开始排烃，晚白垩世末约66 Ma达到生排烃高峰期，之后由于构造抬升作用，生烃作用停止。Baobab C-2井潜山油藏经历了晚白垩世80~55 Ma的原生油气充注阶段和古近纪约30 Ma的次生油气成藏事件。在晚白垩世期间石油的充注表现为充注强度程度不同的连续过程，开始于晚白垩世80 Ma的石油充注事件以较低成熟度原油为主，而发生于约70 Ma的第二期石油充注事件则以成熟油气为主，该期充注事件是形成现今油气分布格局的主要贡献者。古近纪发生的次生成藏事件代表因构造作用而引起油气调整。

关键词: 基岩, 潜山, 油气成藏年代, Bongor盆地, 乍得

Abstract:

Baobab buried-hill reservoir is the major oil reservoir in the north slope of Bongor Basin. Taking Baobab C-2 buried-hill reservoir as an example, its hydrocarbon accumulation history is analyzed and studied in terms of the hydrocarbon generation and expulsion history of source rocks, tectonic thermal evolution history, the GOI characteristics of fluid inclusion, micro-photoluminescence, thermometric techniques and etc. Through studying burial history, it is found that the major source rocks in Mimosa Formation and Prosopis Formation of Baobab area began to generate hydrocarbon at about 90 Ma, and started to expel hydrocarbon at about 80 Ma. At about 66 Ma in the Late Cretaceous, hydrocarbon generation and expulsion reached the peak; afterwards, hydrocarbon generation ceased due to tectonic uplift. Baobab C-2 buried-hill reservoir experienced the primary oil-gas charging stage at about 80-55 Ma in the Late Cretaceous and the secondary hydrocarbon accumulation event at about 30 Ma in Paleocene. In the late Cretaceous period, the oil charging was a continuous process with different degrees of charging intensity. The oil charging event beginning at 80 Ma was dominated by low-maturity crude oil; the second stage of oil charging event happening at 70 Ma was dominated by mature oil and gas, and made a major contribution to the formation of current oil-gas distribution pattern. The occurrence of secondary accumulation event in Paleocene represents the oil-gas adjustment event resulted from tectonism.

Key words: bed rock, buried-hill, hydrocarbon accumulation age, Bongor Basin, Chad

中图分类号:

TE122.1

文志刚, 李威, 窦立荣, 张光亚, 程顶胜, 杜业波, 胡瑛, 王利. Bongor盆地Baobab地区潜山油气成藏期次[J]. 石油学报, 2018, 39(8): 869-875.

Wen Zhigang, Li Wei, Dou Lirong, Zhang Guangya, Cheng Dingsheng, Du Yebo, Hu Ying, Wang Li. Buried-hill hydrocarbon accumulation stage of Baobab area in Bongor Basin[J]. Acta Petrolei Sinica, 2018, 39(8): 869-875.

参考文献

[1] PARNELL J,MIDDLETON D,CHEN Honghan,et al. The use of integrated fluid inclusion studies in constraining oil charge history and reservoir compartmentation:examples from the Jeanne d'Arc Basin,offshore Newfoundland[J].Marine and Petroleum Geology,2001,18(5):535-549.
[2] BOURDET J,PIRONON J,LEVRESSE G,et al.Petroleum accumulation and leakage in a deeply buried carbonate reservoir,Níspero field (Mexico)[J].Marine and Petroleum Geology,2010,27(1):126-142.
[3] BURRUSS R C,CERCONE K R,HARRIS P M.Fluid inclusion petrography and tectonic-burial history of the Al Ali No.2 well:evidence for the timing of diagenesis and oil migration,northern Oman Foredeep[J].Geology,1983,11(10):567-570.
[4] SWARBRICK R E.Reservoir diagenesis and hydrocarbon migration under hydrostatic palaeopressure conditions[J].Clay Minerals,1994,29(4):463-474.
[5] LIU K Y,BOURDET J,ZHANG B S,et al.Hydrocarbon charge history of the Tazhong Ordovician reservoirs,Tarim Basin as revealed from an integrated fluid inclusion study[J].Petroleum Exploration and Development,2013,40(2):183-193.
[6] MARCHAND A M E,SMALLEY P C,HASZELDINE R S,et al.Note on the importance of hydrocarbon fill for reservoir quality prediction in sandstones[J].AAPG Bulletin,2002,86(9):1561-1571.
[7] GEORGE S C,KRIEGER F W,EADINGTON P J,et al.Geochemical comparison of oil-bearing fluid inclusions and produced oil from the Toro sandstone,Papua New Guinea[J].Organic Geochemistry,1997,26(3/4):155-173.
[8] LIU K Y,EADINGTON P.Quantitative fluorescence techniques for detecting residual oils and reconstructing hydrocarbon charge history[J].Organic Geochemistry,2005,36(7):1023-1036.
[9] BODNAR R J,BETHKE P M.Systematics of stretching of fluid inclusions I:fluorite and sphalerite at 1 atmosphere confining pressure[J].Economic Geology,1984,79(1):141-161.
[10] 窦立荣,魏小东,王景春,等.乍得Bongor盆地花岗质基岩潜山储层特征[J].石油学报,2015,36(8):897-904.
DOU Lirong,WEI Xiaodong,WANG Jingchun,et al.Characteristics of granitic basement rock buried-hill reservoir in Bongor Basin,Chad[J].Acta Petrolei Sinica,2015,36(8):897-904.
[11] GUIRAUD R,MAURIN J C.Early cretaceous rifts of western and central Africa:an overview[J]. Tectonophysics,1992,213(1/2):153-168.
[12] GENIK G J.Petroleum geology of Cretaceous-Tertiary rift basins in Niger,Chad,and Central African Republic[J].AAPG Bulletin,1993,77(8):1405-1434.
[13] 窦立荣,肖坤叶,胡勇,等.乍得Bongor盆地石油地质特征及成藏模式[J].石油学报,2011,32(3):379-386.
DOU Lirong,XIAO Kunye,HU Yong,et al.Petroleum geology and a model of hydrocarbon accumulations in the Bongor Basin,the Republic of Chad[J].Acta Petrolei Sinica,2011,32(3):379-386.
[14] 窦立荣,潘校华,田作基,等.苏丹裂谷盆地油气藏的形成与分布——兼与中国东部裂谷盆地对比分析[J].石油勘探与开发,2006,33(3):255-261.
DOU Lirong,PAN Xiaohua,TIAN Zuoji,et al.Hydrocarbon formation and distribution of rift basins in Sudan:a comparative analysis of them with rift basins in East China[J].Petroleum Exploration and Development,2006,33(3):255-261.
[15] 宋红日,窦立荣,肖坤叶,等.Bongor盆地油气成藏地质条件及分布规律初探[J].石油与天然气地质,2009,30(6):762-767.
SONG Hongri,DOU Lirong,XIAO Kunye,et al.An exploratory research on geological conditions of hydrocarbon pooling and distribution patterns of reservoirs in the Bongor Basin[J].Oil & Gas Geology,2009,30(6):762-767.
[16] GREEN P F,DUDDY I R.Thermal history reconstruction in sedimentary basins using apatite fission-track analysis and related techniques[M]//HARRIS N D,PETERS K E.Analyzing the thermal history of sedimentary basins:methods and case histories.SEPM Special Publication,2013,103:65-104.
[17] 肖坤叶,赵健,余朝华,等.中非裂谷系Bongor盆地强反转裂谷构造特征及其对油气成藏的影响[J].地学前缘,2014,21(3):172-180.
XIAO Kunye,ZHAO Jian,YU Zhaohua,et al.Structural characteristics of intensively inversed Bongor Basin in CARS and their impacts on hydrocarbon accumulation[J].Earth Science Frontiers,2014,21(3):172-180.
[18] 路玉林,刘嘉麒,窦立荣,等.非洲乍得盆地玄武岩K-Ar和³⁹Ar-⁴⁰Ar年代学及其动力学背景[J].地质学报,2009,83(8):1125-1133.
LU Yulin,LIU Jiaqi,DOU Lirong,et al.K-Ar and ³⁹Ar-⁴⁰Ar geochronology of basalts from the chad basins,Africa and its geodynamics setting[J].Acta Geologica Sinica,2009,83(8):1125-1133.
[19] 麻伟娇,卫延召,曾德龙,等.准噶尔盆地莫索湾凸起古油藏的流体证据[J].石油学报,2017,38(4):414-424.
MA Weijiao,WEI Yanzhao,ZENG Delong,et al.Fluid evidence of paleo-reservoir in the Mosuowan uplift,Junggar Basin[J].Acta Petrolei Sinica,2017,38(4):414-424.
[20] PIRONON J,BARRES Q.Semi-quantitative FT-IR microanalysis limits:evidence from synthetic hydrocarbon fluid inclusions in sylvite[J].Geochimica et Cosmochimica Acta,1990,54(3):509-518.
[21] 李峰,姜振学,李卓,等.库车坳陷迪北气藏流体包裹体特征及油气充注历史[J].中南大学学报:自然科学版,2016,47(2):515-523.
LI Feng,JIANG Zhenxue,LI Zhuo,et al.Fluid inclusion characteristics and hydrocarbon charge history of Dibei gas reservoir in the Kuqa depression[J].Journal of Central South University:Science and Technology,2016,47(2):515-523.
[22] 陈刚,丁超,徐黎明,等.多期次油气成藏流体包裹体间接定年——以鄂尔多斯盆地东北部二叠系油气藏为例[J].石油学报,2012,33(6):1003-1011.
CHEN Gang,DING Chao,XU Liming,et al.Indirect dating of multi-stage hydrocarbon accumulations by fluid inclusion data:a case study of the Permian hydrocarbon accumulation in the northeast Ordos Basin[J].Acta Petrolei Sinica,2012,33(6):1003-1011.
[23] 白冰,王清斌,赵国祥,等.蓬莱9-1构造新生代构造演化:磷灰石裂变径迹证据[J].石油学报,2015,36(9):1098-1107.
BAI Bing,WANG Qingbin,ZHAO Guoxiang,et al.Cenozoic tectonic evolution of PL9-1 structure:an evidence of apatite fission track[J].Acta Petrolei Sinica,2015,36(9):1098-1107.
[24] 潘雪峰,刘麟.苏北盆地S-F油田烃类流体包裹体红外光谱特征研究[J].天然气勘探与开发,2013,36(3):31-34.
PAN Xuefeng,LIU Lin.IR spectrum of hydrocarbon-fluid inclusion in S-F oilfield,Subei Basin[J].Natural Gas Exploration and Development,2013,36(3):31-34.
[25] 蒋静,张鼐,潘文龙,等.塔里木盆地台盆区奥陶系储层烃包裹体成熟度[J].石油学报,2016,37(5):644-652.
JIANG Jing,ZHANG Nai,PAN Wenlong,et al.Hydrocarbon inclusion maturity of Ordovician reservoirs in craton area of Tarim Basin[J].Acta Petrolei Sinica,2016,37(5):644-652.
[26] 王民,LI Zhongsheng.激光拉曼技术评价沉积有机质热成熟度[J].石油学报,2016,37(9):1129-1136.
WANG Min,LI Zhongsheng.Thermal maturity evaluation of sedimentary organic matter using laser Raman spectroscopy[J].Acta Petrolei Sinica,2016,37(9):1129-1136.
[27] 李威,窦立荣,文志刚,等.乍得Bongor盆地潜山油气成因和成藏过程[J].石油学报,2017,38(11):1253-1262.
LI Wei,DOU Lirong,WEN Zhigang,et al.Buried-hill hydrocarbon genesis and accumulation process in Bongor Basin,Chad[J].Acta Petrolei Sinica,2017,38(11):1253-1262.

Bongor盆地Baobab地区潜山油气成藏期次

Buried-hill hydrocarbon accumulation stage of Baobab area in Bongor Basin

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