深水沉积及海底扇相模式研究进展
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摘要
随着全球油气勘探与开发技术的不断推进,海洋深水区逐渐成为油气勘探的新热点。海底扇作为深水区油气主要储集体,其独特的深水沉积相模式一直是业内人士关注的焦点,而其沉积相模式的复杂性也是研究者久攻不克的难点。从"深水沉积"研究历史及进展着手,分析不同时期"海底扇"理论的成因机理、沉积模式的异同点,总结了深水沉积研究的不断发展与逐步深入的历程,深水海底扇的成因机理、沉积模式仍是需要继续探索解决的海洋石油地质科学中的难点问题,对深水扇沉积内幕结构的认识已经从早期对现象的描述发展到探究其沉积的动力学机理。同时,基于大量岩心、测井与地震资料,越来越多的接近实际的深水海底扇模型得以建立,为深水油气勘探中海底扇储层的有效预测奠定了基础。
With the technologic advancement of oil and gas exploration,deep marine area has become the new hot point gradually.As the main reservoir of the deep water,the exclusive and complex characters of the sedimentary facies model,submarine fan has always been the key topic of depositional experts in the world.On the basic of analysis of the similarities and differences in different periods of "submarine fan" theory and its mechanism,sedimentary model,the characters and improvements of the deep-water sedimentary research are summarized,the study shows that the mechanism and sedimentary mode are difficulties in the offshore petroleum geology field.It is recongnized that sedimentary scientists have already made the most solid step,to the description of the phenomenon and the sedimentary dynamic mechanism during more than a century of research.At the same time,more and more submarine fan modes have been established based on the data of core,logging and seism,which form the effective foundation of reservoir prediction of oil and gas exploration in deep water.
With the technologic advancement of oil and gas exploration,deep marine area has become the new hot point gradually.As the main reservoir of the deep water,the exclusive and complex characters of the sedimentary facies model,submarine fan has always been the key topic of depositional experts in the world.On the basic of analysis of the similarities and differences in different periods of "submarine fan" theory and its mechanism,sedimentary model,the characters and improvements of the deep-water sedimentary research are summarized,the study shows that the mechanism and sedimentary mode are difficulties in the offshore petroleum geology field.It is recongnized that sedimentary scientists have already made the most solid step,to the description of the phenomenon and the sedimentary dynamic mechanism during more than a century of research.At the same time,more and more submarine fan modes have been established based on the data of core,logging and seism,which form the effective foundation of reservoir prediction of oil and gas exploration in deep water.
引文
[1]蒋恕,王华,Weimer P.深水沉积层序特点及构成要素[J].地球科学,2008,33(6):825-833.
[2]庞雄,陈长民,彭大钧,等.南海珠江深水扇系统及油气[J].北京:科学出版社,2007:300-315.
[3]Bouma A H,Normark W R,Barnes N E.COMFAN:Needs and initial results[A].Bouma,A H,Normark,W R,Barnes N E,eds.Submarine fans and related turbidite systems[C].New York:Springer-Verlag,1985:7-12.
[4]王亚辉,赵鹏肖,左倩媚,等.浅析深水沉积理论[J].地质学报,2010,30(2):150-153.
[5]Shanmugam G.Deep-Water Processes and Facies Models:Implications for Sandstone Petroleum Reservoirs[M].Oxford:Elsevier,2006:19-50.
[6]Shanmugam G.50years of turbidite paradigm(1950～1990s):deep-water processes and facies models-a critical perspective[J].Marine and petroleum geology,2000,17(2):285-342.
[7]王英民,王海荣,邱燕,等.深水沉积的动力学机制和响应[J].沉积学报,2007,25(4):495-504.
[8]吴昌荣.南海珠江深水扇系统的内幕结构研究[D].成都:成都理工大学,2007:1-80.
[9]Friedman G M,Sanders J E.Dispelling themyths of seafloor tranquility[J].Geotimes,1997,42:24-27.
[10]李祥辉,王成善,金玮等.深海沉积理论发展及其在油气勘探中的意义[J].沉积学报,2009,27(1):77-86.
[11]Normark W R.Growth Patterns of Deep Sea Fans[J].AAPG Bulletin,1970,54(11):2170-2195.
[12]庞雄,陈长民,朱明,等.深水沉积研究前缘问题[J].地质论评,2007,53(1):36-43.
[13]Shanmugam G.The Bouma Sequence and the turbidite mind set[J].Earth-science reviews,1997,42(4):201-229.
[14]Shanmugam G.Ten turbidite myths[J].Earth-science reviews,2002,58(3):311-341.
[15]张兴阳,罗顺社,何幼斌.沉积物重力流深水牵引流沉积组合-鲍玛序列多解性探讨[J].江汉石油学院学报,2001,23(1):1-5.
[16]周荣福,张莲美,王英民,等.尼日尔三角洲与南海北部陆坡地貌及沉积样式[J].西南石油大学学报(自然科学版),2009,31(3):69-73.
[17]袁圣强,吴时国,马玉波,等.南大西洋深水盆地的构造沉积演化及含油气系统[J].天然气地球科学,2008,19(2):216-221.
[18]姚根顺,袁圣强,吴时国,等.琼东南盆地深水区双物源沉积模式及勘探前景[J].石油勘探与开发,2008,35(6):685-691.
[19]王海荣,王英民,邱燕,等.深水环境多级地貌坡折控制下的重力流动力学的演变[J].地质学报,2009,83(6):812-819.
[20]王海荣,王英民,邱燕,等.南海东北部台湾浅滩陆坡的浊流沉积物波的发育及其成因的构造控制[J].沉积学报,2008,26(1):39-45.
[21]彭大钧,庞雄,陈长民,等.从浅水陆架走向深水陆坡-南海深水扇系统的研究[J].沉积学报,2005,23(1):1-11.
[22]庞雄.南海珠江深水扇系统及其油气勘探前景[J].石油学报,2006,27(3):11-16.
[23]彭大钧,陈长民,庞雄,等.南海珠江口盆地深水扇系统的发现[J].石油学报,2004,25(5):17-23.
[24]李磊,王英民,张莲美,等.南海北部白云深水区水道与朵体沉积序列及演化[J].海洋地质与第四纪地质,2009,29(4):71-76.
[25]李磊,王英民,张莲美,等.尼日尔三角洲坡脚逆冲带沉积样式及构造控制[J].地球科学-中国地质大学学报,2008,33(5):643-650.
[26]高月华.非洲深水区块油气勘探经济评价探析[J].现代商贸工业,2008(12):137-138.
[27]金春爽,乔德武,姜春艳.国内外深水区油气勘探新进展[J].海洋地质动态,2003,19(10):20-23.
[28]Shanmugam G,Walker K R.Tectonic Significance of Distal Turbidites in the Middle Ordovician Block House and Lower SevierFormation in East Tennessee[J].American Journal Science,1978,27(8):551-578.
[29]Nilsen T H.Modern and Ancient Submarine Fans:Discussion of Papers by Walker R G and Normark W R[J].AAPG Bulletin,1980,64(7):1094-1112.
[30]Vail P R.Seismic stratigraphy interpretation using sequence stratigraphy,Part 1[A].Bally A W.Atlas of seismic stratigraphy[C].AAPGStudies in Geology,1987(1):1-10.
[31]Shanmugam G,Moiola R J.Types of submarine fan lobes:models and implications[J].AAPG Bulletin,1991,75(1):156-179.
[32]Reading H G,Richards M.Turbidite Systems in Deep-Water Basin Margings Classified by Grain Size and Feeder System[J].AAPG Bulletin,1994,78(5):792-822.
[33]Richards M,Bowman M.Submarine Fans and Related Depositional Systems II:Variability in Reservoir Architecture and Wireline LogCharacter[J].Marine and Petroleum Geology,1998,15(8):821-839.
[34]Bao Z D.Continental slope limestones of Lower and Middle Triassic,South China[J].Sedimentary Geology,1998,118(1-4):77-93.
[35]Bao Z D.Episodic carbonate deposits on continental slope,the Triassic,South China[J].Acta Geologica Sinica,1999,73(1):93-103.
[36]Stow D A V,Johansson M.Deep-water massive sands:nature,origin and hydrocarbon implications[J].Marine and PetroleumGeology,2000,17(2):145-174.
[2]庞雄,陈长民,彭大钧,等.南海珠江深水扇系统及油气[J].北京:科学出版社,2007:300-315.
[3]Bouma A H,Normark W R,Barnes N E.COMFAN:Needs and initial results[A].Bouma,A H,Normark,W R,Barnes N E,eds.Submarine fans and related turbidite systems[C].New York:Springer-Verlag,1985:7-12.
[4]王亚辉,赵鹏肖,左倩媚,等.浅析深水沉积理论[J].地质学报,2010,30(2):150-153.
[5]Shanmugam G.Deep-Water Processes and Facies Models:Implications for Sandstone Petroleum Reservoirs[M].Oxford:Elsevier,2006:19-50.
[6]Shanmugam G.50years of turbidite paradigm(1950～1990s):deep-water processes and facies models-a critical perspective[J].Marine and petroleum geology,2000,17(2):285-342.
[7]王英民,王海荣,邱燕,等.深水沉积的动力学机制和响应[J].沉积学报,2007,25(4):495-504.
[8]吴昌荣.南海珠江深水扇系统的内幕结构研究[D].成都:成都理工大学,2007:1-80.
[9]Friedman G M,Sanders J E.Dispelling themyths of seafloor tranquility[J].Geotimes,1997,42:24-27.
[10]李祥辉,王成善,金玮等.深海沉积理论发展及其在油气勘探中的意义[J].沉积学报,2009,27(1):77-86.
[11]Normark W R.Growth Patterns of Deep Sea Fans[J].AAPG Bulletin,1970,54(11):2170-2195.
[12]庞雄,陈长民,朱明,等.深水沉积研究前缘问题[J].地质论评,2007,53(1):36-43.
[13]Shanmugam G.The Bouma Sequence and the turbidite mind set[J].Earth-science reviews,1997,42(4):201-229.
[14]Shanmugam G.Ten turbidite myths[J].Earth-science reviews,2002,58(3):311-341.
[15]张兴阳,罗顺社,何幼斌.沉积物重力流深水牵引流沉积组合-鲍玛序列多解性探讨[J].江汉石油学院学报,2001,23(1):1-5.
[16]周荣福,张莲美,王英民,等.尼日尔三角洲与南海北部陆坡地貌及沉积样式[J].西南石油大学学报(自然科学版),2009,31(3):69-73.
[17]袁圣强,吴时国,马玉波,等.南大西洋深水盆地的构造沉积演化及含油气系统[J].天然气地球科学,2008,19(2):216-221.
[18]姚根顺,袁圣强,吴时国,等.琼东南盆地深水区双物源沉积模式及勘探前景[J].石油勘探与开发,2008,35(6):685-691.
[19]王海荣,王英民,邱燕,等.深水环境多级地貌坡折控制下的重力流动力学的演变[J].地质学报,2009,83(6):812-819.
[20]王海荣,王英民,邱燕,等.南海东北部台湾浅滩陆坡的浊流沉积物波的发育及其成因的构造控制[J].沉积学报,2008,26(1):39-45.
[21]彭大钧,庞雄,陈长民,等.从浅水陆架走向深水陆坡-南海深水扇系统的研究[J].沉积学报,2005,23(1):1-11.
[22]庞雄.南海珠江深水扇系统及其油气勘探前景[J].石油学报,2006,27(3):11-16.
[23]彭大钧,陈长民,庞雄,等.南海珠江口盆地深水扇系统的发现[J].石油学报,2004,25(5):17-23.
[24]李磊,王英民,张莲美,等.南海北部白云深水区水道与朵体沉积序列及演化[J].海洋地质与第四纪地质,2009,29(4):71-76.
[25]李磊,王英民,张莲美,等.尼日尔三角洲坡脚逆冲带沉积样式及构造控制[J].地球科学-中国地质大学学报,2008,33(5):643-650.
[26]高月华.非洲深水区块油气勘探经济评价探析[J].现代商贸工业,2008(12):137-138.
[27]金春爽,乔德武,姜春艳.国内外深水区油气勘探新进展[J].海洋地质动态,2003,19(10):20-23.
[28]Shanmugam G,Walker K R.Tectonic Significance of Distal Turbidites in the Middle Ordovician Block House and Lower SevierFormation in East Tennessee[J].American Journal Science,1978,27(8):551-578.
[29]Nilsen T H.Modern and Ancient Submarine Fans:Discussion of Papers by Walker R G and Normark W R[J].AAPG Bulletin,1980,64(7):1094-1112.
[30]Vail P R.Seismic stratigraphy interpretation using sequence stratigraphy,Part 1[A].Bally A W.Atlas of seismic stratigraphy[C].AAPGStudies in Geology,1987(1):1-10.
[31]Shanmugam G,Moiola R J.Types of submarine fan lobes:models and implications[J].AAPG Bulletin,1991,75(1):156-179.
[32]Reading H G,Richards M.Turbidite Systems in Deep-Water Basin Margings Classified by Grain Size and Feeder System[J].AAPG Bulletin,1994,78(5):792-822.
[33]Richards M,Bowman M.Submarine Fans and Related Depositional Systems II:Variability in Reservoir Architecture and Wireline LogCharacter[J].Marine and Petroleum Geology,1998,15(8):821-839.
[34]Bao Z D.Continental slope limestones of Lower and Middle Triassic,South China[J].Sedimentary Geology,1998,118(1-4):77-93.
[35]Bao Z D.Episodic carbonate deposits on continental slope,the Triassic,South China[J].Acta Geologica Sinica,1999,73(1):93-103.
[36]Stow D A V,Johansson M.Deep-water massive sands:nature,origin and hydrocarbon implications[J].Marine and PetroleumGeology,2000,17(2):145-174.
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