巴西坎普斯盆地大油气田成藏特征与分布规律

何娟; 何登发; 李顺利

doi:10.11781/sysydz201105517

巴西坎普斯盆地大油气田成藏特征与分布规律

doi: 10.11781/sysydz201105517

中国地质大学能源学院, 北京, 100083

基金项目: 中国石油天然气股份有限公司重大科技专项(2008E-060903)资助

详细信息

作者简介:
何娟(1987- ),女,硕士研究生,从事石油地质综合研究.E-mail:hejuan326@163.com.

中图分类号: TE122.3⁺3
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出版历程
- 收稿日期: 2010-12-21
- 修回日期: 2011-08-24
- 刊出日期: 2011-10-28

Accumulation and distribution of giant oil and gas fields in Campos Basin, Brazil

School of Energy Resources, China University of Geosciences, Beijing 100083, China

摘要

摘要: 巴西的坎普斯盆地是典型的大西洋型被动大陆边缘盆地,主要经历了裂谷期、过渡期及漂移期3期构造演化,并沉积了与之对应的裂谷期陆相层序、过渡期盐岩层序及漂移期海相层序。其中裂谷期陆相层序中的黑色湖相钙质页岩为盆地中的主力烃源岩,过渡期盐岩层序中的蒸发盐岩将该盆地储集层分隔为盐上和盐下两部分,而漂移期海相层序中发育的浊积砂岩储集着该盆地中90%的已探明油气储量。坎普斯盆地最重要的含油气系统为Lagoa Feia—Carapebus含油气系统,盐下的Lagoa Feia群烃源岩生成的油气通过与盐运动相关的断层运移至盐上Campos群Carapebus组浊积砂岩中储集;油气分布主要受烃源岩的埋深、蒸发盐岩的发育、浊积砂岩的分布以及生长断层的发育等油气地质条件的共同控制。
- 油气成藏特征 /
- 含油气系统 /
- 蒸发盐岩 /
- 坎普斯盆地 /
- 巴西
Abstract: The Campos Basin in Brazil is a typical passive continental margin basin of Atlantic type.It has experienced 3 stages of tectonic evolution including rifting,transitional and drifting,and the corres-ponding sequences of continental facies,evaporate rock and marine facies have been deposited respectively.During the rifting stage,the black lacustrine calcareous shale in the continental sequence worked as the main source rock.The evaporate rocks in the transitional sequence divided the reservoirs in the basin into 2 sections: pre-salt and post-salt.About 90% of the total reserves of the basin have been found in the turbidity sandstones in the marine facies sequence deposited during the drifting stage.The most important petroleum system in the basin is Lagoa Feia-Carapebus.Petroleum generated from the source rocks in Lagoa Feia Group migrated along faults into the turbidity sandstones in Carapebus Formation of Campos Group.Petroleum distribution was mainly controlled by source rock burial depth,evaporate rock generation,turbidity sandstone distribution and fault generation.
- petroleum accumulation feature /
- petroleum system /
- evaporate rock /
- Campos Basin /
- Brazil

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参考文献(19)

[1]	Guardado L,Gamboa L,Lucchesi C.Petroleum geology of the Campos Basin,Brazil,:a model for a producing Atlantic type basin[M] //Edwards J D,Santogrossi P A,eds.Divergent/passive margin basins, AAPG Memoir 48. Tulsa:AAPG,1989:3-80.
[2]	Halbouty M.Giant oil and gas fields of the decade 1990-1999,AAPG Memoir 78[M].Tulsa:AAPG,2003:15-105.
[3]	Uchupi E.The tectonic style of the Atlantic Mesozoic rift system[J]. Journal of African Earth Sciences, 1989,8(2-4):143-164.
[4]	Dickson W G,Fryklund R E,Odegard M E,et al.Constraints 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(3-4):309-322.
[5]	Meisling K,Cobbold P,Mount V.Segmentation of an obliquely rifted margin,Campos and Santos basins,southeastern Brazil[J].AAPG Bulletin,2001,85 (11):1903-1924.
[6]	Mohriak W,Macedo J,Castellani R,et al.Salt tectonics and structural styles in the deep-water province of the Cabo Frio region,Rio de Janeiro,Brazil[M] //Jackson M P A,Roberts D G,Snelson S.Salt tectonics:a global perspective,AAPG Memoir 65.Tulsa:AAPG,1995:204-273.
[7]	Rangel H,Paulo DE Tarso M,Spadini A.Barracuda and Roncador giant oil fields,deep-water Campos Basin,Brazil[M] //Halbouty M.Giant oil and gas fields of the decade 1990-1999.Tulsa:AAPG,2003:123-137.
[8]	Mello M,Telnaes N,Gaglianone P,et al.Organic geochemical eharacterisation of depositional palaeoenvironments of source rocks and oils in Brazilian marginal basins[J].Organic Geochemistry,1988,13(1-3):31-45.
[9]	Mohriak W,Hobbs R,Dewey J.Basin-forming processes and the deep structure of the Campos Basin,offshore Brazil[J].Marine and Petroleum Geology,1990,7(2):94-100.
[10]	Trindade L,Soldan A,Cerqueira J,et al.Petroleum generation,migration,and accumulation in deep water area of Campos Basin,Brazil[M].Tulsa:AAPG,1990:781.
[11]	Mello M R,Trinidade L A F,Rangel A V O,et al.Comparative geochemical characterization of Latin American oils derived from Devonian to Miocene source rocks:a biological marker and isotope approach[C] // Mello M R,Trinidade L A F,Hessel M H R,eds.ALAGO Special Publication.Fourth Latin American Congress on Organic Geochemistry,Bucaramanga,Colombia,October 1994,Extended Abstracts:109-112.
[12]	Guardado L,Spadini A,Brand O J,et al.Petroleum system of the Campos Basin,Brazil[M] //Mello M,Katz B.Petroleum Systems of South Atlantic Margins,AAPG Memoir 73.Tulsa:AAPG,2000:317-324.
[13]	Peters K,Waiters C,Moldowan J.The biomarker guide[M].Cambridge,UK:Cambridge University Press,2005:1-1155.
[14]	Mello M,Koutsoukos E,Mohriak W,et al.Selected petroleum systems in Brazil[M] //Magoon L,Dow W. MemoirsAmerican Association of Petroleum Geologists.Tulsa:AAPG,1994:499-512.
[15]	Pimentel A,Gomes R.The basic igneous rocks as a reservoir of Badejo Field,Campos Basin:proceedings of the 3th Brazilian Petroleum Congress[C].1982.
[16]	Abrahao D,Warme J.Lacustrine and associated deposits in a rifted continental margin:Lower Cretaceous Lagoa Feia Formation,Campos Basin,offshore Brazil[M] //Katz B.Lacustrine basin exploration:case studies and modern analogs,AAPG Memoir 50.Tulsa:AAPG,1990:287-305.
[17]	Peres W.Shelf-fed turbidite system model and its application to the Oligocene deposits of the Campos Basin,Brazil[J].AAPG Bulletin,1996,77(1):81-101.
[18]	Cobbold P,Meisling K,Mount V.Reactivation of an obliquely rifted margin,Campos and Santos basins,southeastern Brazil [J]. AAPG Bulletin, 2001,85 (11):1925-1944.
[19]	Soldan A,Cerqueira J,Ferreira J,et al.Aspects related to the habitat of the oil fields of Marlin and Albacora-bacia in Campos basin[J].Internal Report,Petrobras/CRNPES/DIVEX/SEGEQ,1990:170.