TRAP CHARACTERISTICS OF THE MAIN DEEP-WATER BASINS IN THE WORLD
-
摘要: 通过对巴西东部大陆边缘地区、西非被动大陆边缘地区、墨西哥湾地区及澳大利亚西北大陆架地区共15个深水盆地圈闭类型的归纳分析,总结出深水盆地具有构造圈闭、地层圈闭和复合圈闭3大类共8种圈闭类型,其中以构造圈闭为主,包括背斜圈闭、断层圈闭和盐体刺穿圈闭;墨西哥湾盆地、巴西坎波斯盆地和桑托斯盆地及西非地区的阿尤恩-塔尔法亚盆地、塞内加尔盆地、Rio Muni盆地、加蓬盆地、下刚果盆地和宽扎盆地均为含盐盆地,盐岩的运动形成大量的底辟拱升背斜圈闭,盐体刺穿圈闭和与盐运动相关的地层圈闭及复合圈闭。Abstract: Based on the analysis of fifteen deep-water basins which situated in the eastern Brazilian continental margin, West African passive continental margin, Gulf of Mexico and the Northwest Shelf of Australia, the article sums up three major trap types i.e. structural trap, stratigraphic trap and compound trap and there are eight trap styles included in these three types. The structural trap which include anticlinal trap, fault trap and salt diapir trap are most important. The traps in the Gulf of Mexico Basin, Campos Basin and Santos Basin in Brazil, Aaiun-Tarfaya Basin, Senegal Basin, Rio Muni Basin, Gabon Basin, Lower Congo Basin and Kwanza Basin in West Africa are all with salt. The tectonic movement of the salt generates abundant diapir anticlinal traps, salt diapir traps, stratigraphic traps and compound traps which are relevant with salt movement.
-
Key words:
- deep-water basin /
- structural trap /
- stratigraphic trap /
- compound trap /
- salt structure
-
-
[1] 爱德华A博蒙特, 诺曼H福斯特. 油气圈闭勘探[M]. 北京:石油工业出版社, 2002:22-54.[Edward A Beaumont, Norman H Foster. Exploration of hydrocarbon traps[M]. Beijing:Petroleum Industry Press, 2002:22
-54.]
[2] [3] 陈春峰. 世界深水勘探特点及中国深水勘探现状分析[J]. 石油天然气学报, 2005, 27(6):835-837.
[CHEN Chunfeng. Characters of world deep-water exploration and current situation of deep-water exploration in China[J]. Journal of Oil and Gas Technology, 2005, 27(6):835-837.]
[4] 李国玉, 金之钧. 世界含油气盆地图集[M]. 北京:石油工业出版社, 2005:249-334, 599-654.
[LI Guoyu, JIN Zhijun. World Atlas of Oil and Gas Basins[M]. Beijing:Petroleum Industry Press, 2005:249-334, 599-654.]
[5] 夏义平, 黄忠范, 袁秉衡, 等. 世界巨型油气田[M]. 北京:石油工业出版社, 2007:15-58.[XIA Yiping, HUANG Zhongfan, YUAN bingheng, et al. Giant Fields in the World[M]. Beijing:Petroleum Industry Press, 2007, 15
-58.]
[6] Deptuck M E, Steffens G S, Barton M D, et al. Architecture and evolution of upper fan channel belts on the Niger Delta slope and in the Arabian Sea[J]. Marine and Petroleum Geology, 2003, (20):649-676.
[7] Galloway W E. Growth faults and fault-related structures of prograding terrigenous clastic continental margins[J]. Gulf Coast Association of Geological Societies Transactions, 1986, (36):121-128.
[8] Dickson W G. Constrains for plate reconstruction using gravity data-implications for source and reservoir distribution in Brazilian and West African margin basins[J]. Marine and Petroleum Geology, 2003, (20):309-323.
[9] Alexander B, R Kagi, G Woodhouse. Origin of the oil, Barrow Island, Western Australia[J]. Australia Petroleum Exploration Association Journal, 1980, 20(1):250-256.
[10] Jackson M P A. Role of subaerial volcanic rocks and mantle plumes in creation of South Atlantic margins:implications for salt tectonics and source rocks[J]. Marine and Petroleum Geology, 2000, (17):477-498.
[11] Kirk R B. Seismic stratigraphic cycles in the eastern Barrow sub-basin, Northwest Shelf, Australia[J]. Australian Society of Exploration Geophysicists and Australian Petroleum Geophysics Symposium, 1984, 437-479.
[12] Kennard J M, Deighton I, Edwards D S. Subsidence and thermal history modelling:New insights into hydrocarbon expulsion from multiple petroleum systems in the Petrel Sub-basin, Bonaparte Basin[C]//. From Sedimentary Basins of Western Australia, 409-437.
[13] Crostella A, T Barter. Triassic/Jurassic depositional history of the Dampier and Beagle sub-basins, Northwest Shelf of Australia[J]. Australian Petroleum Exploration Association Journal, 1980, 20(1):25-33.
[14] Dolby J H, B E Balme. Triassic reservoir bed of the Carnarvon basin, Western Australia[J]. Review of Palaeobotany and Palynology, 1976, (22):195-198.
[15] Kamer G D. Tectonic significance of syn-rift sediment packages across the Gabon-Cabana continental margin[J]. Marine and Petroleum Geology, 1997, 7(4):973-1000.
[16] Bur wood, R Angola. Source rock control for Lower Congo Coastal and Kwanza Basin petroleum systems, in Cameron[J]:Geological Society Special Publication, 1999, (153):81-194.
[17] Hudec M R, Jackson M P A. Regional restoration across the Kwanza Basin, Angola:Salt tectonics triggered by repeated uplift of a metastable passive margin[J]. AAPG Bulletin, 2004, 88(7):971-990.
[18] Hudec M R. Structural segmentation, inversion, and salt tectonics on a passive margin:Evolution of the Inner Kwanza Basin, Angola[J]. Geological Society of America, 2002, 114(10):1222-1244.
[19] Fort X. Salt tectonics on the Angolan margin, syn-sedimentary deformation processes[J]. AAPG, 2004, 88(11):1423-1544.
[20] Bird D E, Burke K, Hall S A. Gulf of Mexico tectonic history:Hot spot tracks, crustal boundaries, and early salt distribution[J]. 2005, AAPG Bulletin, 89(3):311-328.
[21] Echols D J, Curtis D M. Paleontologic evidence for mid-Miocene refrigeration, from subsurface marine shale[J]. AAPG Bulletin, 1973, 57(12):776-777.
[22] Goldhammer R K, Johnson C A. Middle Jurassic-Upper Cretaceous paleogeographic evolution and sequence-stratigraphic framework of the northwest Gulf of Mexico[C]//:The western Gulf of Mexico Basin:Tectonics, sedimentary basins, and petroleum systems. AAPG Bulletin, 2001, (75):45-81.
[23] Fillon R H, Lawless P N. Lower Miocene-early Pliocene deposystems in the Gulf of Mexico:Regional sequence relationships[J]. Gulf Coast Association of Geological Societies Transactions, 2000, (50):411-428.
[24] Weimer P, Rowan M G., McBride B C, et al. Evaluating the petroleum systems of the northern deep gulf of Mexico through integrated basin analysis[J]. AAPG Bulletin, 1998, 82(5B):865-877.
[25] Hall S H. The role of autochthonous salt inflation and deflation in the northern Gulf of Mexico[J]. Marine and Petroleum Geology, 2002, (19):649-682.
[26] Liro L M. Comparison of allochthonous salt deformation and sub-salt structural styles, Perdido and Mississippi Fan fold belts, deepwater Gulf of Mexico[J]. Gulf Coast Association of Geological Societies Transactions, 2002, (52):621-629.
[27] Dorthe Moller Hansen, Jonathan Redfern. Miocene igneous activity in the Northern Sub-basin, offshore Senegal, NW Africa[J], Marine and Petroleum Geology, 2008, (25):1-15.
[28] Mello M R, Kotsoukos E A M, Mohriak W U. Selected petroleum systems in Brazil[C]//:The petroleum system-from source to trap. AAPG Bulletin, 1994, 60(2):499-512.
[29] Viana A R, Faugeres J C, Kowsmann R O, et al. Morphology and sedimentology of the Campos continental margin, offshore Brazil[J]. Sedimentary Geology, 1998, (115):133-157.
[30] Cobbold P R, Meisling K E. Reactivation of an obliquely-rifted margin, Campos and Santos basins, southeastern Brazil[J]. AAPG Bulletin, 2001, 11(85):1925-1944.
[31] Carlos H L Bruhhn, Roger G Walker. High-resolution stratigraphy and sedimentary evolution of coarse-grained canyon-filling turbidites from the Upper Cretaceous transgressive megasequence, Campos basin, offshore Brazil[J]. Jounary of Sedimentary Research, 1995, 4(5):426-442.
[32] Caddah L F, Kowsmann R O. Slope sedimentary facies associated with Pleistocene and Holocene sea-level changes, Campos Basin, Southeast Brazilian Margin[J]. Sedimentary Geology, 1998, 115:159-174.
[33] Demerciam S, Szatmari P, Cobhold P R. Style and pattern of salt diapirs due to thin skinned gravitational sliding, Campos and Santos basins, offshore Brazil[J]. AAPG Bulletin, 1993, 228(34):393-433.
[34] Broucke F Temple. The role of deformation processes on the geometry of mud-dominated turbiditic systems, Oligocene and Lower-Middle Miocene of the Lower Congo basin (West African Margin)[J]. Marine and Petroleum Geology, 2004, (21):327-348.
[35] Cole G A, Ormerod D, Smith J. Predicting oil charge types and quality in the deepwater offshore lower Congo Basin, Angola[J]. AAPG Bulletin, 1998, (82):190-200.
[36] Turner J P, Rosendahl B R, Wilson P G. Structure and evolution of an obliquely sheared continental margin:Rio Muni, West Africa[J]. Tectonophysics, 2003, (37):41-55.
[37] Jennette D, Fouad K, Grimaldo F, et al. Traps and turbidite reservoir characteristics from a complex and evolving tectonic setting, Veracruz Basin, southeastern Mexico[J]:AAPG Bulletin, 2003, 87(10):1599-1622.
[38] Modica C J. Postrift sequence stratigraphy, paleogeography and fill history of the deep-water Santos basin, offshore southeast Brazil[J]. AAPG Bulletin. 2004, 88(7):923-945.
-
计量
- 文章访问数: 1313
- PDF下载数: 3
- 施引文献: 0
下载: