松辽盆地徐家围子断陷营城组粗面岩成因与隐爆机制
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摘要
松辽盆地徐家围子断陷营城组火山岩中含有粗面质岩石,是深层天然气重要储层之一。岩心、钻井及地震资料研究表明,粗面岩具有高位喷发、低位充填的特征,在火山口附近厚度大,远离火山口厚度小。粗面岩主量、微量及同位素地球化学显示其属于钾玄岩系列,富集稀土元素,强不相容元素Rb、Ba、Th、U质量分数较高。粗面岩的(87Sr/86Sr)i=0.704 321～0.705 395,εNd(t)为正值(3.36～3.83),Pb同位素比值相对集中,(206Pb/204Pb)i、(207Pb/204Pb)i、(208Pb/204Pb)i平均值分别为18.43、15.51和38.23。研究表明,粗面质岩浆由区域年轻地壳组分部分熔融形成,经历了一定程度的分离结晶作用,地壳混染作用不显著。粗面质岩浆多期次喷发后形成粗面岩,热液气体不断聚集发生隐蔽爆破形成角砾,未固结的角砾被岩浆期后热液"胶结",形成隐爆角砾岩,构成了粗面质岩石重要的储层类型。
Trachyte is one of the important deep-gases reservoirs among volcanic rocks in Yingcheng Formation of Xujiaweizi fault depression,Songliao basin.Core,drill and seismic data exhibit that trachyte always erupt at higher location and flow to low-lying areas.In general,the thickness increases toward crater.Major element,trace element and isotopic geochemistry studies indicate that the trachyte belongs to shoshonitic series.The trachyte are prominently enriched strongly incompatible elements such as Rb,Ba,Th,U,REE,and have low initial 87Sr/86Sr(0.704321-0.705395) ratios.All εNd(t) values of the trachyte are all positive and have a narrow range(3.36-3.83),but they have an analogical radiogenic Pb.The mean of(206Pb/204Pb)i,(207Pb/204Pb)i,(208Pb/204Pb)i are 18.43,15.51 and 38.23,respectively.The features of geochemical data indicate that the trachyte magma are derived from partial melting juvenile crust following fractional crystallization without crustal contamination.Hydrothermal gases continuously gather into trachyte after many times eruptions.The trachytes would be crypto-explosive when the pressure is not large enough to bear.The crypto-explosive breccias are formed when the autobreccias are cemented by hydrothermal fluids,which can creat many cracks and inter-granular space.
Trachyte is one of the important deep-gases reservoirs among volcanic rocks in Yingcheng Formation of Xujiaweizi fault depression,Songliao basin.Core,drill and seismic data exhibit that trachyte always erupt at higher location and flow to low-lying areas.In general,the thickness increases toward crater.Major element,trace element and isotopic geochemistry studies indicate that the trachyte belongs to shoshonitic series.The trachyte are prominently enriched strongly incompatible elements such as Rb,Ba,Th,U,REE,and have low initial 87Sr/86Sr(0.704321-0.705395) ratios.All εNd(t) values of the trachyte are all positive and have a narrow range(3.36-3.83),but they have an analogical radiogenic Pb.The mean of(206Pb/204Pb)i,(207Pb/204Pb)i,(208Pb/204Pb)i are 18.43,15.51 and 38.23,respectively.The features of geochemical data indicate that the trachyte magma are derived from partial melting juvenile crust following fractional crystallization without crustal contamination.Hydrothermal gases continuously gather into trachyte after many times eruptions.The trachytes would be crypto-explosive when the pressure is not large enough to bear.The crypto-explosive breccias are formed when the autobreccias are cemented by hydrothermal fluids,which can creat many cracks and inter-granular space.
引文
[1]Schutter S R.Hydrocarbon Occurrence and Explora-tion in and Around Igneous Rocks[J].Geological Soci-ety,London,Special Publications,2003,214:7-33.
[2]刘嘉麒,孟凡超,崔岩,等.试论火山岩油气藏成藏机理[J].岩石学报,2010,26(1):1-13.Liu Jiaqi,Meng Fanchao,Cui Yan,et al.Discussionon the Relationship Between Volcanism and PetroleumAccumulation[J].Acta Petrologica Sinica,26(1):1-13.
[3]Magara K.Volcanic Reservoir Rocks of NorthwesternHonshu Island,Japan[J].Geological Society,London,Special Publications,2003,214:69-81.
[4]邱隆伟,姜在兴,席庆福.欧利坨子地区沙三下亚段火山岩成岩作用及孔隙演化[J].石油与天然气地质,2000,21(2):139-147.Qiu Longwei,Jiang Zaixing,Xi Qingfu.Diagenesisand Pore Evolution of Lower Es3Volcanic Rocks inOulituozi Region[J].Oil and Gas Geology,2000,21(2):139-147.
[5]Gu L X,Ren Z W,Wu C Z,et al.Hydrocarbon Res-ervoirs in a Trachyte Porphyry Intrusion in the EasternDepression of the Liaohe Basin,Northeast China[J].AAPG Bull,2002,86(10):1821-1832.
[6]操应长,姜在兴,邱隆伟.山东惠民凹陷商741块火成岩油藏储集空间类型及形成机理探讨[J].岩石学报,1999,15(1):129-136.Cao Yingchang,Jiang Zaixing,Qiu Longwei.Studyon the Type and Origin of the Reservoir Space of Igne-ous Oil Oeservoir in Shang 741Block,Huimin Depres-sion,Shandong[J].Acta Petrologica Sinica,1999,15(1):129-136.
[7]Dutkiewicz A,Volk H,Ridley J,et al.Geochemistryof Oil in Fluid Inclusions in a Middle Proterozoic Igne-ous Intrusion:Implications for the Source of Hydro-carbons in Crystalline Rocks[J].Organic Geochemis-try,2004,35(8):937-957.
[8]Petford N,Mccaffery K J W.Hydrocarbons in Crys-talline Rocks:An Introduction[J].Geological Society,London,Special Publications,2003,214:1-5.
[9]王璞珺,冯志强.盆地火山岩:岩性、岩相、储层、气藏、勘探[M].北京:科学出版社,2008.Wang Pujun,Feng Zhiqiang.Volcanic Rocks in Petro-liferous Basin:Petrography,Facies,Reservoir,Pool,Exploration[M].Beijing:Science Press,2008.
[10]黄玉龙,王璞珺,舒萍,等.松辽盆地营城组中基性火山岩储层特征及成储机理[J].岩石学报,2010,26(1):82-92.Huang Yulong,Wang Pujun,Shu Ping,et al.Char-acteristics and Formation Mechasism of the Creta-ceous Intermediate and Mafic Volcanic Reservoir inSongliao Basin,NE China[J].Acta Petrologica Sini-ca,2010,26(1):82-92.
[11]姜传金,陈树民,初丽兰,等.徐家围子断陷营城组火山岩分布特征及火山喷发机制的新认识[J].岩石学报,2010,26(1):63-72.Jiang Chuanjin,Chen Shumin,Chu Lilan,et al.ANew Understanding About the Volcanic DistributionCharacteristics and Eruption Mechanism of YingchengFormation in Xujiaweizi Fault Depression[J].ActaPetrologica Sinica,2010,26(1):63-72.
[12]Wang P J,Ren Y G,Shan X L,et al.The Creta-ceous Volcanic Succession Around the Songliao Ba-sin,NE China:Relationship Between Volcanism andSedimentation[J].Geological Journal,2002,37:97-115.
[13]Feng Z Q.Volcanic Rocks as Prolific Gas Reservoir:A Case Study from the Qingshen Gas Field in theSongliao Basin,NE China[J].Marine and PetroleumGeology 2008,25:416-432.
[14]Le Bas M J,Le Maitre R W,Streckeisen A,et al.AChemical Classification of Volcanic Rocks Based onthe Total Alkali-Silica Diagram[J].Journal of Petro-logy,1986,27:745-750.
[15]Wang P J,Chen F K,Chen S M,et al.Geochemicaland Nd-Sr-Pb Isotopic Composition of Mesozoic Vol-canic Rocks in the Songliao Basin,NE,China[J].Ge-ochemical Journal,2006,40:149-159.
[16]章凤奇.松辽盆地北部早白垩世火山事件与地球动力学[D].杭州:浙江大学,2007.Zhang Fengqi.Early Cretaceous Volcanic Events inthe Northern Songliao Basin and Its Geodynamics[D].Hangzhou:Zhejiang University,2007.
[17]章凤奇,程晓敢,陈汉林,等.松辽盆地东南缘晚中生代火山事件的锆石年代学与地球化学制约[J].岩石学报,2009,25(1):39-54.Zhang Fengqi,Cheng Xiaogan,Chen Hanlin,et al.Zircon Chronological and Geochemical Constraints onthe Late Mesozoic Volcanic Events in the Southeast-ern Margin of the Songliao Basin,NE China[J].ActaPetrologica Sinica,2009,25(1):39-54.
[18]陈井胜.松辽盆地南部营城组火山岩成因[D].长春:吉林大学,2009.Chen Jingsheng.The Genesis of Volcanic Rocks ofYingcheng Group in Southern Songliao Basin[D].Changchun:Jilin University,2009.
[19]宋立忠,赵泽辉,焦贵浩,等松辽盆地早白垩世火山岩地球化学特征及其构造意义[J].岩石学报,2010,26(4):1182-1194.Song Lizhong,Zhao Zehui,Jiao Guihao,et al.Geo-chemical Characteristics of Early Cretaceous VolcanicRocks from Songliao Basin,Northeast China,and ItsTectonic Implications[J].Acta Petrologica Sinica,2010,26(4):1182-1194.
[20]Anders E,Grevesse N.Abundances of the Elements:Meteoritic and Solar[J].Geochimica et CosmochimicaActa,1989,53:197-214.
[21]Sun S S,McDonough W F.Chemical and IsotopicSystematics of Oceanic Basalts:Implications forMantle Composition and Processes[C]//Saunders AD,Norry M J.Magmatism in the Ocean Basins.[s.l.]:Geological Society Special Publication,1989:313-345.
[22]李龙,郑永飞,周建波.中国大陆地壳铅同位素演化的动力学模型[J].岩石学报,2001,17(1):61-68.Li Long,Zheng Yongfei,Zhou Jianbo.DynamicModel for Pb Isotope Evolution in the ContinentalCrust of China[J].Acta Petrologica Sinica,2001,17(1):61-68.
[23]Riley T R,Leat P T,Pankhurst R J,et al.Originsof Large Volume Rhyolitic Volcanism in the AntarcticPeninsula and Patagonia by Crustal Melting[J].Jour-nal of Petrology,2001,42(6):1043-1065.
[24]Hofmann A W.Nd in Hawaiian Magmas:Constraintson Source Compositionand Evolution[J].ChemicalGeology,1986,57:17-30.
[25]Campbell I H.Implications of Nb/U,Th/U and Sm/Nd in Plume Magmas for the Relationship BetweenContinental and Oceanic Crust Formation and the De-pleted Mantle[J].Geochemica et Cosmochimica Ac-ta,2002,66(9):1651-1661.
[26]Deng J F,Zhao H L,Luo Z H.Mantle Plumes andLithosphere Motion in East Asia[C]//Flower M,Chung S L,Lo C H,et al.Mantle Dynamics andPlate Interactions in East Asia.[s.l.]:America Geo-physics Union Geodynamics,1998:59-65.
[27]吴昌志,顾连兴,任作伟,等.辽河盆地沙三期火山-侵入岩地球化学与岩石成因[J].岩石学报,2004,20(3):545-556.Wu Changzhi,Gu Lianxing,Ren Zuowei,et al.Geo-chemistry and Petrogenesis of Eocene Volcanic-Intru-sive Rocks in Liaohe Basin,Northeastern China[J].Acta Petrologica Sinica,2003,20(3):545-556.
[28]Vijaya Kumar K,Frost C D,Frost B R,et al.TheChimakurti,Errakonda,and Uppalapadu Plutons,Eastern Ghats Belt,India:An Unusual Associationof Tholeiitic and Alkaline Magmatism[J].Lithos,2007,97(1/2):30-57.
[29]Su S G,Niu Y L,Deng J F,et al.Petrology and Ge-ochronology of Xuejiashiliang Igneous Complex andTheir Genetic Link to the Lithospheric Thinning Dur-ing the Yanshanian Orogenesis in Eastern China[J].Lithos,2007,96(1/2):90-107.
[30]Mingram B,Trumbull R B,Littman S,et al.A Petro-genetic Study of Anorogenic Felsic Magmatism in theCretaceous Paresis Ring Complex,Namibia:Evi-dence for Mixing of Crust and Mantle-Derived Com-ponents[J].Lithos,2000,54(1/2):1-22.
[31]项媛馨,巫建华.广东北部早白垩世粗面岩的成因:Sr-Nd-Pb同位素制约[J].高校地质学报,2011,17(3):436-446.Xiang Yuanxin,Wu Jianhua.Origin of the Early Cre-taceous Trachyte in Northern Guangdong ProvinceConstraints of Sr-Nd-Pb Isotopes[J].GeologicalJournal of China Universities,2011,17(3):436-446.
[32]Wu F Y,Jahn B M,Wilde S A,et al.Highly Frac-tionated I-Type Granites in NE China:I:Geochronolo-gy and Petrogenesis[J].Lithos,2003,66(3/4):241-273.
[33]孟凡超,刘嘉麒,李明,等.松辽盆地徐家围子营城组流纹岩地球化学特征及构造指示意义[J].岩石学报,2010,26(1):227-241.Meng Fanchao,Liu Jiaqi,Li Ming,et al.Geochemistryand Tectonic Implications of Rhyolites fromYingcheng Formation in Xujiaweizi,Songliao Basin[J].Acta Petrologica Sinica,2010,26(1):227-241.
[34]Montel J M,Vielzeuf D.Partial Melting of Gray-wackes:PartⅡ:Compostion of Mineral and Melts[J].Contributions to Mineralogy and Petrology,1997,128:176-196.
[35]Litvinovsky B A,Steele I M,Wickham S M.SilicicMagma Formation in Overthickened Crust:Meltingof Charnockite and Leucogranite at 15,20and 25kbar[J].Journal of Petrology,2000,41:717-737.
[36]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,2003,10(3):51-59.Wu Fuyuan,Ge Wenchun,Sun Deyou,et al.Discus-sions on the Lithospheric Thinning Eastern China[J].Earth Science Frontiers,2003,10(3):51-59.
[37]周济元,崔炳芳,陈世忠,等.江西会昌红山隐爆角砾岩筒及其成因和动力学[J].成都理工学院学报,1998,25(2):261-268.Zhou Jiyuan,Cui Bingfang,Chen Shizhong,et al.The Cryptoexplosive Breccia and Its Origin and Dy-namics in Hongshan,Huichang Country,JiangxiProvince[J].Journal of Chengdu University of Tech-nology,1998,25(2):261-268.
[38]王照波.隐爆岩及其形成模式探讨[J].地质找矿论丛,2001,16(3):201-204.Wang Zhaobo.Discussion of Cryto Explosive Rocksand the Formation Model[J].Contribution to Geolo-gy and Mineral Resources Research,2001,16(3):201-204.
[39]Sillitoe R H.Ore-Related Breccias in VolcanoplutonicAres[J].Economic Geology,1985,80:1467-1514.
[40]梁俊红,巩恩普,姚玉增,等.中酸性隐爆角砾岩型金属矿床稀土元素地球化学特征[J].地质找矿论丛,2011,26(1):23-27.Liang Junhong,Gong Enpu,Yao Yuzeng,et al.TheREE Geochemical Characteristics of Intermediate-Acid Crytoexplosive Breccia-Type Metalliferous De-posit[J].Contribution to Geology and Mineral Re-sources Research,2011,26(1):23-27.
[41]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):525-530.Wu Changzhi,Gu Lianxing,Ren Zuowei,et al.For-mation Mechanism of Hydrocarbon Reservoirs Rela-ted to Igneous Rocks in Mesozoic-Cenozoic Basin,Eastern China[J].Acta Geologica Sinica,2005,79(4):525-530.
[42]Jackson J A.Glossary of Geology[M].Virginia:A-merican Geological Institute,1997.
[43]王璞珺,陈树民,李伍志,等.松辽盆地白垩纪火山期后热液活动的岩石地球化学和年代学及其地质意义[J].岩石学报,2010,26(1):33-46.Wang Pujun,Chen Shumin,Li Wuzhi,et al.,Chro-nology,Petrology and Geochemistry of the Creta-ceous Cryto-Exlosive Breccia-Bearing VolcanicRocks:Implications for Volcanic Reservoir and Tec-tonics of the Songliao Basin,NE China[J].ActaPetrologica Sinica,2010,26(1):33-46.
[44]王璞珺,迟元林,刘万洙,等.松辽盆地火山岩相:类型、特征和储层意义[J].吉林大学学报:地球科学版,2003,33(4):449-456.Wang Pujun,Chi Yuanlin,Liu Wanzhu,et al.Vol-canic Facies of the Songliao Basin:Classification,Characteristics and Reservoirs Significance[J].Jour-nal of Jilin University:Earth Science Edition,2003,33(4):449-456.
[2]刘嘉麒,孟凡超,崔岩,等.试论火山岩油气藏成藏机理[J].岩石学报,2010,26(1):1-13.Liu Jiaqi,Meng Fanchao,Cui Yan,et al.Discussionon the Relationship Between Volcanism and PetroleumAccumulation[J].Acta Petrologica Sinica,26(1):1-13.
[3]Magara K.Volcanic Reservoir Rocks of NorthwesternHonshu Island,Japan[J].Geological Society,London,Special Publications,2003,214:69-81.
[4]邱隆伟,姜在兴,席庆福.欧利坨子地区沙三下亚段火山岩成岩作用及孔隙演化[J].石油与天然气地质,2000,21(2):139-147.Qiu Longwei,Jiang Zaixing,Xi Qingfu.Diagenesisand Pore Evolution of Lower Es3Volcanic Rocks inOulituozi Region[J].Oil and Gas Geology,2000,21(2):139-147.
[5]Gu L X,Ren Z W,Wu C Z,et al.Hydrocarbon Res-ervoirs in a Trachyte Porphyry Intrusion in the EasternDepression of the Liaohe Basin,Northeast China[J].AAPG Bull,2002,86(10):1821-1832.
[6]操应长,姜在兴,邱隆伟.山东惠民凹陷商741块火成岩油藏储集空间类型及形成机理探讨[J].岩石学报,1999,15(1):129-136.Cao Yingchang,Jiang Zaixing,Qiu Longwei.Studyon the Type and Origin of the Reservoir Space of Igne-ous Oil Oeservoir in Shang 741Block,Huimin Depres-sion,Shandong[J].Acta Petrologica Sinica,1999,15(1):129-136.
[7]Dutkiewicz A,Volk H,Ridley J,et al.Geochemistryof Oil in Fluid Inclusions in a Middle Proterozoic Igne-ous Intrusion:Implications for the Source of Hydro-carbons in Crystalline Rocks[J].Organic Geochemis-try,2004,35(8):937-957.
[8]Petford N,Mccaffery K J W.Hydrocarbons in Crys-talline Rocks:An Introduction[J].Geological Society,London,Special Publications,2003,214:1-5.
[9]王璞珺,冯志强.盆地火山岩:岩性、岩相、储层、气藏、勘探[M].北京:科学出版社,2008.Wang Pujun,Feng Zhiqiang.Volcanic Rocks in Petro-liferous Basin:Petrography,Facies,Reservoir,Pool,Exploration[M].Beijing:Science Press,2008.
[10]黄玉龙,王璞珺,舒萍,等.松辽盆地营城组中基性火山岩储层特征及成储机理[J].岩石学报,2010,26(1):82-92.Huang Yulong,Wang Pujun,Shu Ping,et al.Char-acteristics and Formation Mechasism of the Creta-ceous Intermediate and Mafic Volcanic Reservoir inSongliao Basin,NE China[J].Acta Petrologica Sini-ca,2010,26(1):82-92.
[11]姜传金,陈树民,初丽兰,等.徐家围子断陷营城组火山岩分布特征及火山喷发机制的新认识[J].岩石学报,2010,26(1):63-72.Jiang Chuanjin,Chen Shumin,Chu Lilan,et al.ANew Understanding About the Volcanic DistributionCharacteristics and Eruption Mechanism of YingchengFormation in Xujiaweizi Fault Depression[J].ActaPetrologica Sinica,2010,26(1):63-72.
[12]Wang P J,Ren Y G,Shan X L,et al.The Creta-ceous Volcanic Succession Around the Songliao Ba-sin,NE China:Relationship Between Volcanism andSedimentation[J].Geological Journal,2002,37:97-115.
[13]Feng Z Q.Volcanic Rocks as Prolific Gas Reservoir:A Case Study from the Qingshen Gas Field in theSongliao Basin,NE China[J].Marine and PetroleumGeology 2008,25:416-432.
[14]Le Bas M J,Le Maitre R W,Streckeisen A,et al.AChemical Classification of Volcanic Rocks Based onthe Total Alkali-Silica Diagram[J].Journal of Petro-logy,1986,27:745-750.
[15]Wang P J,Chen F K,Chen S M,et al.Geochemicaland Nd-Sr-Pb Isotopic Composition of Mesozoic Vol-canic Rocks in the Songliao Basin,NE,China[J].Ge-ochemical Journal,2006,40:149-159.
[16]章凤奇.松辽盆地北部早白垩世火山事件与地球动力学[D].杭州:浙江大学,2007.Zhang Fengqi.Early Cretaceous Volcanic Events inthe Northern Songliao Basin and Its Geodynamics[D].Hangzhou:Zhejiang University,2007.
[17]章凤奇,程晓敢,陈汉林,等.松辽盆地东南缘晚中生代火山事件的锆石年代学与地球化学制约[J].岩石学报,2009,25(1):39-54.Zhang Fengqi,Cheng Xiaogan,Chen Hanlin,et al.Zircon Chronological and Geochemical Constraints onthe Late Mesozoic Volcanic Events in the Southeast-ern Margin of the Songliao Basin,NE China[J].ActaPetrologica Sinica,2009,25(1):39-54.
[18]陈井胜.松辽盆地南部营城组火山岩成因[D].长春:吉林大学,2009.Chen Jingsheng.The Genesis of Volcanic Rocks ofYingcheng Group in Southern Songliao Basin[D].Changchun:Jilin University,2009.
[19]宋立忠,赵泽辉,焦贵浩,等松辽盆地早白垩世火山岩地球化学特征及其构造意义[J].岩石学报,2010,26(4):1182-1194.Song Lizhong,Zhao Zehui,Jiao Guihao,et al.Geo-chemical Characteristics of Early Cretaceous VolcanicRocks from Songliao Basin,Northeast China,and ItsTectonic Implications[J].Acta Petrologica Sinica,2010,26(4):1182-1194.
[20]Anders E,Grevesse N.Abundances of the Elements:Meteoritic and Solar[J].Geochimica et CosmochimicaActa,1989,53:197-214.
[21]Sun S S,McDonough W F.Chemical and IsotopicSystematics of Oceanic Basalts:Implications forMantle Composition and Processes[C]//Saunders AD,Norry M J.Magmatism in the Ocean Basins.[s.l.]:Geological Society Special Publication,1989:313-345.
[22]李龙,郑永飞,周建波.中国大陆地壳铅同位素演化的动力学模型[J].岩石学报,2001,17(1):61-68.Li Long,Zheng Yongfei,Zhou Jianbo.DynamicModel for Pb Isotope Evolution in the ContinentalCrust of China[J].Acta Petrologica Sinica,2001,17(1):61-68.
[23]Riley T R,Leat P T,Pankhurst R J,et al.Originsof Large Volume Rhyolitic Volcanism in the AntarcticPeninsula and Patagonia by Crustal Melting[J].Jour-nal of Petrology,2001,42(6):1043-1065.
[24]Hofmann A W.Nd in Hawaiian Magmas:Constraintson Source Compositionand Evolution[J].ChemicalGeology,1986,57:17-30.
[25]Campbell I H.Implications of Nb/U,Th/U and Sm/Nd in Plume Magmas for the Relationship BetweenContinental and Oceanic Crust Formation and the De-pleted Mantle[J].Geochemica et Cosmochimica Ac-ta,2002,66(9):1651-1661.
[26]Deng J F,Zhao H L,Luo Z H.Mantle Plumes andLithosphere Motion in East Asia[C]//Flower M,Chung S L,Lo C H,et al.Mantle Dynamics andPlate Interactions in East Asia.[s.l.]:America Geo-physics Union Geodynamics,1998:59-65.
[27]吴昌志,顾连兴,任作伟,等.辽河盆地沙三期火山-侵入岩地球化学与岩石成因[J].岩石学报,2004,20(3):545-556.Wu Changzhi,Gu Lianxing,Ren Zuowei,et al.Geo-chemistry and Petrogenesis of Eocene Volcanic-Intru-sive Rocks in Liaohe Basin,Northeastern China[J].Acta Petrologica Sinica,2003,20(3):545-556.
[28]Vijaya Kumar K,Frost C D,Frost B R,et al.TheChimakurti,Errakonda,and Uppalapadu Plutons,Eastern Ghats Belt,India:An Unusual Associationof Tholeiitic and Alkaline Magmatism[J].Lithos,2007,97(1/2):30-57.
[29]Su S G,Niu Y L,Deng J F,et al.Petrology and Ge-ochronology of Xuejiashiliang Igneous Complex andTheir Genetic Link to the Lithospheric Thinning Dur-ing the Yanshanian Orogenesis in Eastern China[J].Lithos,2007,96(1/2):90-107.
[30]Mingram B,Trumbull R B,Littman S,et al.A Petro-genetic Study of Anorogenic Felsic Magmatism in theCretaceous Paresis Ring Complex,Namibia:Evi-dence for Mixing of Crust and Mantle-Derived Com-ponents[J].Lithos,2000,54(1/2):1-22.
[31]项媛馨,巫建华.广东北部早白垩世粗面岩的成因:Sr-Nd-Pb同位素制约[J].高校地质学报,2011,17(3):436-446.Xiang Yuanxin,Wu Jianhua.Origin of the Early Cre-taceous Trachyte in Northern Guangdong ProvinceConstraints of Sr-Nd-Pb Isotopes[J].GeologicalJournal of China Universities,2011,17(3):436-446.
[32]Wu F Y,Jahn B M,Wilde S A,et al.Highly Frac-tionated I-Type Granites in NE China:I:Geochronolo-gy and Petrogenesis[J].Lithos,2003,66(3/4):241-273.
[33]孟凡超,刘嘉麒,李明,等.松辽盆地徐家围子营城组流纹岩地球化学特征及构造指示意义[J].岩石学报,2010,26(1):227-241.Meng Fanchao,Liu Jiaqi,Li Ming,et al.Geochemistryand Tectonic Implications of Rhyolites fromYingcheng Formation in Xujiaweizi,Songliao Basin[J].Acta Petrologica Sinica,2010,26(1):227-241.
[34]Montel J M,Vielzeuf D.Partial Melting of Gray-wackes:PartⅡ:Compostion of Mineral and Melts[J].Contributions to Mineralogy and Petrology,1997,128:176-196.
[35]Litvinovsky B A,Steele I M,Wickham S M.SilicicMagma Formation in Overthickened Crust:Meltingof Charnockite and Leucogranite at 15,20and 25kbar[J].Journal of Petrology,2000,41:717-737.
[36]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,2003,10(3):51-59.Wu Fuyuan,Ge Wenchun,Sun Deyou,et al.Discus-sions on the Lithospheric Thinning Eastern China[J].Earth Science Frontiers,2003,10(3):51-59.
[37]周济元,崔炳芳,陈世忠,等.江西会昌红山隐爆角砾岩筒及其成因和动力学[J].成都理工学院学报,1998,25(2):261-268.Zhou Jiyuan,Cui Bingfang,Chen Shizhong,et al.The Cryptoexplosive Breccia and Its Origin and Dy-namics in Hongshan,Huichang Country,JiangxiProvince[J].Journal of Chengdu University of Tech-nology,1998,25(2):261-268.
[38]王照波.隐爆岩及其形成模式探讨[J].地质找矿论丛,2001,16(3):201-204.Wang Zhaobo.Discussion of Cryto Explosive Rocksand the Formation Model[J].Contribution to Geolo-gy and Mineral Resources Research,2001,16(3):201-204.
[39]Sillitoe R H.Ore-Related Breccias in VolcanoplutonicAres[J].Economic Geology,1985,80:1467-1514.
[40]梁俊红,巩恩普,姚玉增,等.中酸性隐爆角砾岩型金属矿床稀土元素地球化学特征[J].地质找矿论丛,2011,26(1):23-27.Liang Junhong,Gong Enpu,Yao Yuzeng,et al.TheREE Geochemical Characteristics of Intermediate-Acid Crytoexplosive Breccia-Type Metalliferous De-posit[J].Contribution to Geology and Mineral Re-sources Research,2011,26(1):23-27.
[41]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):525-530.Wu Changzhi,Gu Lianxing,Ren Zuowei,et al.For-mation Mechanism of Hydrocarbon Reservoirs Rela-ted to Igneous Rocks in Mesozoic-Cenozoic Basin,Eastern China[J].Acta Geologica Sinica,2005,79(4):525-530.
[42]Jackson J A.Glossary of Geology[M].Virginia:A-merican Geological Institute,1997.
[43]王璞珺,陈树民,李伍志,等.松辽盆地白垩纪火山期后热液活动的岩石地球化学和年代学及其地质意义[J].岩石学报,2010,26(1):33-46.Wang Pujun,Chen Shumin,Li Wuzhi,et al.,Chro-nology,Petrology and Geochemistry of the Creta-ceous Cryto-Exlosive Breccia-Bearing VolcanicRocks:Implications for Volcanic Reservoir and Tec-tonics of the Songliao Basin,NE China[J].ActaPetrologica Sinica,2010,26(1):33-46.
[44]王璞珺,迟元林,刘万洙,等.松辽盆地火山岩相:类型、特征和储层意义[J].吉林大学学报:地球科学版,2003,33(4):449-456.Wang Pujun,Chi Yuanlin,Liu Wanzhu,et al.Vol-canic Facies of the Songliao Basin:Classification,Characteristics and Reservoirs Significance[J].Jour-nal of Jilin University:Earth Science Edition,2003,33(4):449-456.
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