沉积盆地火成构造研究综述
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摘要
岩浆活动在沉积盆地中是非常广泛的。随着油气勘探领域的扩展,对沉积盆地火成岩及相关构造的研究愈加重要。沉积盆地火成构造是指在沉积盆地中由岩浆侵入或喷发作用形成的岩浆和围岩及上覆层变形构造的总和。当前,利用三维地震数据研究岩席的几何学与侵位机制取得了重要进展,开启了沉积盆地火成构造研究的新时代。三维地震分析是沉积盆地火成构造研究强有力的手段。加强火成构造的研究不仅可以深化对沉积盆地构造的认识,也可以深化对火成构造圈闭的认识,为寻找与火成岩相关的油气藏提供了新思路。
Magmatic activity is widespread in sedimentary basins world-wide.As hydrocarbon exploration spreads to igneous rocks,the understanding of the role of igneous complexes in the basin is becomes increasingly important.Basinal igneous tectonics is defined here as the deformations involving igneous complexes,host rocks and overburden resulted from magma intrusion and extrusion.Recently,the study of geometry and emplacement mechanisms of igneous sills by using 3D seismic reflection data has made great achievements,which has started a new ear of igneous tectonic analysis.Interpretation of 3D reflection seismic data offers a novel approach to the understanding of the fundamental aspects and hydrocarbon implications of basinal igneous tectonics.The research of igneous tectonics is one of the key fundamental problems of structural analysis in sedimentary basins,and is of broad practice prospecting in the petroleum exploration.A better understanding of the igneous rocks will improve our understanding of basinal structures and hydrocarbon traps related igneous rocks,and bring a number of new ideas of hydrocarbon exploration.
Magmatic activity is widespread in sedimentary basins world-wide.As hydrocarbon exploration spreads to igneous rocks,the understanding of the role of igneous complexes in the basin is becomes increasingly important.Basinal igneous tectonics is defined here as the deformations involving igneous complexes,host rocks and overburden resulted from magma intrusion and extrusion.Recently,the study of geometry and emplacement mechanisms of igneous sills by using 3D seismic reflection data has made great achievements,which has started a new ear of igneous tectonic analysis.Interpretation of 3D reflection seismic data offers a novel approach to the understanding of the fundamental aspects and hydrocarbon implications of basinal igneous tectonics.The research of igneous tectonics is one of the key fundamental problems of structural analysis in sedimentary basins,and is of broad practice prospecting in the petroleum exploration.A better understanding of the igneous rocks will improve our understanding of basinal structures and hydrocarbon traps related igneous rocks,and bring a number of new ideas of hydrocarbon exploration.
引文
[1]Archer S G,Bergman S C,Iliffe J,et al.Palaeogene igneousrocks reveal new insights into the geodynamic evolution and petro-leum potential of the Rockall Trough,NE Atlantic Margin[J].Basin Research,2005,17:171-201.
[2]Rohrman M.Prospectivity of volcanic basins:Trap delineation andacreage de-risking[J].AAPG Bulletin,2007,91(6):915-939.
[3]Jackson MP A.Retrospective salt tectonics[C]∥Jackson MP A,Roberts D G,Snelson S,eds.Salt Tectonics:A Global Perspec-tive.AAPG Memoir65,1995:1-28.
[4]Tao Kuiyuan.Structure Geology of Volcanic Facies[M].Nanjing:Scientific and Technical Press of Jiangsu,1994:1-254.[陶奎元.火山岩相构造学[M].南京:江苏科学技术出版社,1994:1-254.]
[5]Guo Ying,Li Zhiling.Structure Geology Concise Course[M].Wuhan:China University of Geosciences Press,1995:151-161.[郭颖,李智陵.构造地质学简明教程[M].武汉:中国地质大学出版社,1995:151-161.]
[6]Cartwright J,Huuse M.3D seismic technology:The geologicHubble′[J].Basin Research,2005,17:1-20.
[7]Davies R,Bell B R,Cartwright J A,et al.Three dimensionalseismic imaging of Paleogene dike-fed submarine volcanoes fromthe northeast Atlantic margin[J].Geology,2002,30:223-226.
[8]Trude K J.Kinematic indicators for shallow level igneous intru-sions from3D seismic data:Evidence of flow direction and feederlocation[C]∥Davies R J,Cartwright J,Stewart S A,et al.,eds.3D Seismic Technology:Application to the Exploration of Sedi-mentary Basins.London:Geological Society,2004,29:209-217.
[9]Hansen D M,Cartwright J,Thomas D.3D seismic analysis of thegeometry of igneous sills and sill junction relationships[C]∥Da-vies R J,Cartwright J,Stewart S A,et al.,eds.3D SeismicTechnology:Application to the Exploration of Sedimentary Basins.London:Geological Society,2004,29:199-208.
[10]Thomson K,Hutton D.Geometry and growth of sill complexes:Insights using3D seismic from the north Rockall Trough[J].Bul-letin ofVolcanology,2004,66:364-375.
[11]Polteau S,Mazzini A,Galland O,et al.Saucer-shaped intru-sions:Occurrences,emplacement and implications[J].Earthand Planetary Science Letters,2008,266:195-204.
[12]Hansen D M,Cartwright J.The three-dimensional geometry andgrowth of forced folds above saucer-shaped sills[J].Journal ofStructural Geology,2006,28:1 520-1 535.
[13]Trude K J,Cartwright J A,Davies R J,et al.A new techniquefor dating igneous sills[J].Geology,2003,31:813-816.
[14]Hansen D M,Cartwright J.Saucer-shaped sill with lobate mor-phology revealed by 3D seismic data:Implications for resolving ashallow-level sill emplacement mechanism[J].Journal ofthe Ge-ological Society,2006,163:509-523.
[15]Svensen H,Plank S,Malthe-Sφenssen A,et al.Release ofmethane from a volcanic basin as a mechanism for initial Eoceneglobal warming[J].Nature,2004,429:542-545.
[16]Galland O,Cobbold P R,Hallot E,et al.Use of vegetable oiland silica powder for scale modelling of magmatic intrusion in adeforming brittle crust[J].Earth and Planetary Science Letters,2006,243:786-804.
[17]Mathieu L,van Wyk de Vries B,Holohan E P,et al.Dykes,cups,saucers and sills:Analogue experiments on magma intru-sion into brittle rocks[J].Earth and Planetary Science Letters,2008,271:1-13.
[18]Galland O,Planke S,Neumann Else-R,et al.Experimentalmodelling of shallowmagma emplacement:Application to saucer-shaped intrusions[J].Earth and Planetary Science Letters,2009,277:373-383.
[19]Evans R J,DavieswR J,Stewartz S A.Internal structure and e-ruptive history of a kilometer-scale mud volcano system[J].BasinResearch,2006,19:153-163.
[20]Planke S.Seismic volcanostratigraphy of large-volume basaltic ex-trusive complexes on rifted margins[J].Journal ofGeophysicalResearch,2000,105(B8):19 335-19 351.
[21]Rey S S,Planke S,Symonds P A,et al.Seismic volcanostratigra-phy of the Gascoyne margin,western Australia[J].Journal ofVolcanology and Geothermal Research,2008,172:112-131.
[22]Schutter S R.Hydrocarbon occurrence and exploration in and a-round igneous rocks[C]∥Petford N,McCaffrey K J W,eds.Hydrocarbons in Crystalline Rocks.Geological Society of SpecialPublication,2003,214:7-33.
[23]Lee G H,Kwon Y I,Yoon C S,et al.Igneous complexes in theeastern northern south YellowSea Basin and their implications forhydrocarbon systems[J].Marine and Petroleum Geology,2006,23:631-645.
[24]Sun Zhixin.The physical modeling on the structures resulted byigneous rock irruption[J].Petroleum Geophysics,2007,29(3):324-328.[孙志信.火成岩侵入形成的构造物理模拟实验及实例[J].石油实验地质,2007,29(3):324-328.]
[25]Chen Jianwen.A rising borderline science—Volcanic rock reser-voir geology[J].Marine Geology Letters,2002,18(4):19-22.[陈建文.一门新兴的边缘科学———火山岩储层地质学[J].海洋地质动态,2002,18(4):19-22.]
[26]Wang Ling,Sun Xiping,Zhang Yan,et al.Volcanic massif ge-neticm echanism and volcanic facies controlled by deep zone faul-ted systems in Songliao Basin:A case in Xushen area[J].Natu-ral Gas Geosience,2007,18(3):389-393.[王玲,孙夕平,张研,等.松辽盆地深层断裂体系对火山岩成因和火山岩相带的控制:以徐深地区为例[J].天然气地球科学,2007,18(3):389-393.]
[27]Tang Huafeng,Wang Pujun,Jiang Chuanjin,et al.Seismiccharacters of volcanic facies and their distribution relation todeep faults in Songliao Basin[J].Journal ofJilin University(Earth Science Edition),2007,31(7):73-78.[唐华风,王璞君,姜传金,等.松辽盆地火山岩相地震特征及其与控陷断裂的关系[J].吉林大学学报:地球科学版,2007,31(7):73-78.]
[28]Xiao Shangbin,Jiang Zaixing,Cao Yingchang,et al.A prelimi-nary approach to the classification of oil and gas reservoirs in ig-neous rocks[J].Experimental Petroleum Geology,1999,21(4):324-327.[肖尚斌,姜在兴,操应长,等.火成岩油气藏分类初探[J].石油实验地质,1999,21(4):324-327.]
[29]Zhou Lihong,Wu Yongping,Xiao Dunqing,et al.Characteristicof the tertiary igneous rocks and investigation of their relationshipswith hydrocarbon in Huanghua depression[J].Acta Petrolei Sini-ca,2000,21(6):29-34.[周立宏,吴永平,肖敦清,等.黄骅坳陷第三系火成岩与油气关系探讨[J].石油学报,2000,21(6):29-34.]
[30]Wu Changzhi,Gu Lianxing,Ren Zuowei,et al.Formationmechanism of hydrocarbon reservoirs related to igneous rocks inMesozoic-Cenozoic Basin,eastern China[J].Acta GeologicaSinica,2005,79(4):522-530.[吴昌志,顾连兴,任作伟,等.中国东部中、新生代含油气盆地火成岩油气藏成藏机制[J].地质学报,2005,79(4):522-530.]
[2]Rohrman M.Prospectivity of volcanic basins:Trap delineation andacreage de-risking[J].AAPG Bulletin,2007,91(6):915-939.
[3]Jackson MP A.Retrospective salt tectonics[C]∥Jackson MP A,Roberts D G,Snelson S,eds.Salt Tectonics:A Global Perspec-tive.AAPG Memoir65,1995:1-28.
[4]Tao Kuiyuan.Structure Geology of Volcanic Facies[M].Nanjing:Scientific and Technical Press of Jiangsu,1994:1-254.[陶奎元.火山岩相构造学[M].南京:江苏科学技术出版社,1994:1-254.]
[5]Guo Ying,Li Zhiling.Structure Geology Concise Course[M].Wuhan:China University of Geosciences Press,1995:151-161.[郭颖,李智陵.构造地质学简明教程[M].武汉:中国地质大学出版社,1995:151-161.]
[6]Cartwright J,Huuse M.3D seismic technology:The geologicHubble′[J].Basin Research,2005,17:1-20.
[7]Davies R,Bell B R,Cartwright J A,et al.Three dimensionalseismic imaging of Paleogene dike-fed submarine volcanoes fromthe northeast Atlantic margin[J].Geology,2002,30:223-226.
[8]Trude K J.Kinematic indicators for shallow level igneous intru-sions from3D seismic data:Evidence of flow direction and feederlocation[C]∥Davies R J,Cartwright J,Stewart S A,et al.,eds.3D Seismic Technology:Application to the Exploration of Sedi-mentary Basins.London:Geological Society,2004,29:209-217.
[9]Hansen D M,Cartwright J,Thomas D.3D seismic analysis of thegeometry of igneous sills and sill junction relationships[C]∥Da-vies R J,Cartwright J,Stewart S A,et al.,eds.3D SeismicTechnology:Application to the Exploration of Sedimentary Basins.London:Geological Society,2004,29:199-208.
[10]Thomson K,Hutton D.Geometry and growth of sill complexes:Insights using3D seismic from the north Rockall Trough[J].Bul-letin ofVolcanology,2004,66:364-375.
[11]Polteau S,Mazzini A,Galland O,et al.Saucer-shaped intru-sions:Occurrences,emplacement and implications[J].Earthand Planetary Science Letters,2008,266:195-204.
[12]Hansen D M,Cartwright J.The three-dimensional geometry andgrowth of forced folds above saucer-shaped sills[J].Journal ofStructural Geology,2006,28:1 520-1 535.
[13]Trude K J,Cartwright J A,Davies R J,et al.A new techniquefor dating igneous sills[J].Geology,2003,31:813-816.
[14]Hansen D M,Cartwright J.Saucer-shaped sill with lobate mor-phology revealed by 3D seismic data:Implications for resolving ashallow-level sill emplacement mechanism[J].Journal ofthe Ge-ological Society,2006,163:509-523.
[15]Svensen H,Plank S,Malthe-Sφenssen A,et al.Release ofmethane from a volcanic basin as a mechanism for initial Eoceneglobal warming[J].Nature,2004,429:542-545.
[16]Galland O,Cobbold P R,Hallot E,et al.Use of vegetable oiland silica powder for scale modelling of magmatic intrusion in adeforming brittle crust[J].Earth and Planetary Science Letters,2006,243:786-804.
[17]Mathieu L,van Wyk de Vries B,Holohan E P,et al.Dykes,cups,saucers and sills:Analogue experiments on magma intru-sion into brittle rocks[J].Earth and Planetary Science Letters,2008,271:1-13.
[18]Galland O,Planke S,Neumann Else-R,et al.Experimentalmodelling of shallowmagma emplacement:Application to saucer-shaped intrusions[J].Earth and Planetary Science Letters,2009,277:373-383.
[19]Evans R J,DavieswR J,Stewartz S A.Internal structure and e-ruptive history of a kilometer-scale mud volcano system[J].BasinResearch,2006,19:153-163.
[20]Planke S.Seismic volcanostratigraphy of large-volume basaltic ex-trusive complexes on rifted margins[J].Journal ofGeophysicalResearch,2000,105(B8):19 335-19 351.
[21]Rey S S,Planke S,Symonds P A,et al.Seismic volcanostratigra-phy of the Gascoyne margin,western Australia[J].Journal ofVolcanology and Geothermal Research,2008,172:112-131.
[22]Schutter S R.Hydrocarbon occurrence and exploration in and a-round igneous rocks[C]∥Petford N,McCaffrey K J W,eds.Hydrocarbons in Crystalline Rocks.Geological Society of SpecialPublication,2003,214:7-33.
[23]Lee G H,Kwon Y I,Yoon C S,et al.Igneous complexes in theeastern northern south YellowSea Basin and their implications forhydrocarbon systems[J].Marine and Petroleum Geology,2006,23:631-645.
[24]Sun Zhixin.The physical modeling on the structures resulted byigneous rock irruption[J].Petroleum Geophysics,2007,29(3):324-328.[孙志信.火成岩侵入形成的构造物理模拟实验及实例[J].石油实验地质,2007,29(3):324-328.]
[25]Chen Jianwen.A rising borderline science—Volcanic rock reser-voir geology[J].Marine Geology Letters,2002,18(4):19-22.[陈建文.一门新兴的边缘科学———火山岩储层地质学[J].海洋地质动态,2002,18(4):19-22.]
[26]Wang Ling,Sun Xiping,Zhang Yan,et al.Volcanic massif ge-neticm echanism and volcanic facies controlled by deep zone faul-ted systems in Songliao Basin:A case in Xushen area[J].Natu-ral Gas Geosience,2007,18(3):389-393.[王玲,孙夕平,张研,等.松辽盆地深层断裂体系对火山岩成因和火山岩相带的控制:以徐深地区为例[J].天然气地球科学,2007,18(3):389-393.]
[27]Tang Huafeng,Wang Pujun,Jiang Chuanjin,et al.Seismiccharacters of volcanic facies and their distribution relation todeep faults in Songliao Basin[J].Journal ofJilin University(Earth Science Edition),2007,31(7):73-78.[唐华风,王璞君,姜传金,等.松辽盆地火山岩相地震特征及其与控陷断裂的关系[J].吉林大学学报:地球科学版,2007,31(7):73-78.]
[28]Xiao Shangbin,Jiang Zaixing,Cao Yingchang,et al.A prelimi-nary approach to the classification of oil and gas reservoirs in ig-neous rocks[J].Experimental Petroleum Geology,1999,21(4):324-327.[肖尚斌,姜在兴,操应长,等.火成岩油气藏分类初探[J].石油实验地质,1999,21(4):324-327.]
[29]Zhou Lihong,Wu Yongping,Xiao Dunqing,et al.Characteristicof the tertiary igneous rocks and investigation of their relationshipswith hydrocarbon in Huanghua depression[J].Acta Petrolei Sini-ca,2000,21(6):29-34.[周立宏,吴永平,肖敦清,等.黄骅坳陷第三系火成岩与油气关系探讨[J].石油学报,2000,21(6):29-34.]
[30]Wu Changzhi,Gu Lianxing,Ren Zuowei,et al.Formationmechanism of hydrocarbon reservoirs related to igneous rocks inMesozoic-Cenozoic Basin,eastern China[J].Acta GeologicaSinica,2005,79(4):522-530.[吴昌志,顾连兴,任作伟,等.中国东部中、新生代含油气盆地火成岩油气藏成藏机制[J].地质学报,2005,79(4):522-530.]
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