关于发展洋板块地质学的思考
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摘要
为揭示造山带物质组成和结构构造,发展洋板块地质学,阐明大陆形成演化过程和动力来源,应用板块构造理论和地质学方法,对造山带俯冲增生杂岩带、蛇绿岩带等大洋岩石圈板块地质建造、结构构造进行系统研究,寻找俯冲带岛弧前弧火成岩组合;研究洋板块初始俯冲过程中,从前弧玄武岩到玻安岩、高镁安山岩,再到弧拉斑玄武岩和钙碱性熔岩的岩浆作用分阶段递进演变历史,以揭示洋盆向大陆转化的原始弧性质和前弧火成岩组合及洋陆转换过程,为建立和发展洋板块地质学奠定科学基础.
In order to reveal the material composition and the structure of the orogenic belt,we propose the ocean plate geology,which is used to explain the process of continental formation and evolution and the source of dynamics.Based on the theory of plate tectonics and geological research methods,the subduction-accretionary complex,the ophiolite belt,and other oceanic lithospheric plate geological formations and structure construction in the orogenic belt are systematically studied in order to find the igneous rock association of the front arc in the subduction zone.In the initial subduction process of the ocean plate,the magmatism from the forearc basalts(FAB) to the boninite,high-Mg andesite(HMA),to the arc tholeiite and calc-alkaline lava and its different stage evolution,are studied in order to identify the characteristics of the original arc and front arc igneous rock association,which reveals the ocean-continent transition in the evolution process from ocean basin to the continent,laying a scientific foundation for the establishment and development of ocean plate geology.
In order to reveal the material composition and the structure of the orogenic belt,we propose the ocean plate geology,which is used to explain the process of continental formation and evolution and the source of dynamics.Based on the theory of plate tectonics and geological research methods,the subduction-accretionary complex,the ophiolite belt,and other oceanic lithospheric plate geological formations and structure construction in the orogenic belt are systematically studied in order to find the igneous rock association of the front arc in the subduction zone.In the initial subduction process of the ocean plate,the magmatism from the forearc basalts(FAB) to the boninite,high-Mg andesite(HMA),to the arc tholeiite and calc-alkaline lava and its different stage evolution,are studied in order to identify the characteristics of the original arc and front arc igneous rock association,which reveals the ocean-continent transition in the evolution process from ocean basin to the continent,laying a scientific foundation for the establishment and development of ocean plate geology.
引文
Bao,P.S.,Su,L.,Wang,J.,et al.,2015.The Yarlung Zangbo Ophiolite.Geological Publishing House,Beijing,227-233(in Chinese).
Bierlein,F.P.,Groves,D.I.,Cawood,P.A.,2009.Metallogeny of Accretionary Orogens-The Connection between Lithospheric Processes and Metal Endowment.Ore Geology Reviews,36:282-292.
Bierlein,F.P.,Groves,D.I.,Goldfarb,R.J.,et al.,2006.Lithospheric Controls on the Formation of Provinces Hosting Giant Orogenic Gold Deposits.Mineralium Deposita,40:874-887.
Chen,C.,Mao,X.W.,Hu,Z.X.,et al.,2017.Discovery of~817Ma Oceanic Island Basalts in the Dahongshan Region,Northern Hubei Province and Its Significance.Geological Science and Technology Information,36(6):22-31(in Chinese with English abstract).
Cheng,Y.Q.,Wang,H.Z.,2006.A Dictionary of Earth Science:Basic Sciences.Geological Publishing House,Beijing,794(in Chinese).
Dilek,Y.,Furnes,H.,2011.Ophiolite Genesis and Global Tectonics:Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere.Geological Society of America Bulletin,123(3-4):387-411.https://doi.org/10.1130/b30446.1
Dilek,Y.,Robinson,P.T.,2003.Ophiolites in Earth History.Geological Society,London,Special Publications,218:9-19.
Feng,Y.M.,Zhang,Y.,2018.Introduction and Commentary on Ocean Plate Stratigrapgy.Geological Bulletin of China,37(4):523-531(in Chinese with English abstract).
Herrington,R.J.,Brown,D.,2011.The Generation and Preservation of Mineral Deposits in Arc-Continent Collision Environments.Frontiers in Earth Sciences,(Chapter 6):145-159.https://doi.org/10.1007/978-3-540-88558-0
Hu,Z.X.,Mao,X.W.,Tian,W.X.,et al.,2015.Discovery of the Jinningian Orogenic Belt on the Northern Margin of Yangtze Craton in Mountain Dahong.Geological Survey of China,2(2):33-39(in Chinese with English abstract).
Huang,J.Q.,Chen,B.W.,1987.The Evolution of the Tethys in China and Adjacent Regions.Geological Publishing House,Beijing,71-74(in Chinese).
Hutchison,J.S.,Goldman,B.D.,1975.The Relationship between the Rat of Testosterone Infusion and Gonadotropin Secretion.Endocrinology,97(3):725-730.
Isozaki,Y.,Maruyama,S.,Furuoka,F.,1990.Accreted Oceanic Materials in Japan.Tectonophysics,181(1-4):179-205.https://doi.org/10.1016/0040-1951(90)90016-2
Kong,L.Y.,Mao,X.W.,Chen,C.,et al.,2017.Chronological Study on Detrital Zircons and Its Geological Significance from Mesoproterozoic Dagushi Group in the Dahongshan Area,North Margin of the Yangtze Block.Earth Science,42(4):485-501(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.039
Kusky,T.M.,Windley,B.F.,Safonova,I.,et al.,2013.Recognition of Ocean Plate Stratigraphy in Accretionary Orogens through Earth History:A Record of 3.8Billion Years of Sea Floor Spreading,Subduction,and Accretion.Gondwana Research,24(2):501-547.https://doi.org/10.1016/j.gr.2013.01.004
Li,S.G.,2016.Astronomy,Geology,Palaeontology.Geological Publishing House,Beijing,127-134(in Chinese).
Li,T.D.,1998.Polymetallic Nodules.In:Chen,S.P.,ed.,Earth System Science.China Science and Technology Press,Beijing,420(in Chinese).
Li,T.D.,2010.The Works of Li Tingdong.Geological Publishing House,Beijing,1246(in Chinese with English abstract).
Li,Z.X.,2015.Summary of Tectonic Evolution in South China:Plate Tectonics,Geological Events and Resource Effects.Science Publishing House,Beijing,54-88(in Chinese).
Maruyama,S.,Kawai,T.,Windley,B.F.,2010.Ocean Plate Stratigraphy and Its Imbrication in an Accretionary Orogen:The Mona Complex,Anglesey-Lleyn,Wales,UK.Geological Society,London,Special Publications,338(1):55-75.https://doi.org/10.1144/sp338.4
Mo,J.,2004.Frotiers on Marine Geoscience.China Ocean Press,Beijing(in Chinese).
Pan,G.T,Xiao,Q.H.,2016.Explanatory Note to the Tectonic Map of China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Safonova,I.,Biske,G.,Romer,R.L.,et al.,2016.Middle Paleozoic Mafic Magmatism and Ocean Plate Stratigraphy of the South Tianshan,Kyrgyzstan.Gondwana Research,30:236-256.https://doi.org/10.1016/j.gr.2015.03.006
Safonova,I.Y.,Santosh,M.,2014.Accretionary Complexes in the Asia-Pacific Region:Tracing Archives of Ocean Plate Stratigraphy and Tracking Mantle Plumes.Gondwana Research,25(1):126-158.https://doi.org/10.1016/j.gr.2012.10.008
Wakita,K.,Metcalfe,I.,2005.Ocean Plate Stratigraphy in East and Southeast Asia.Journal of Asian Earth Sciences,24(6):679-702.https://doi.org/10.1016/j.jseaes.2004.04.004
Wang,X.B.,Bao,P.S.,Deng,W.M.,et al.,1987.The Ophiolite in Tibet.Geological Publishing House,Beijing(in Chinese).
Xiao,Q.H.,Li,T.D.,Pan,G.T.,et al.,2016.Petrologic Ideas for Identification of Ocean-Continent Transition:Recognition of Intra-Oceanic Arc and Initial Subduction.Geology in China,43(3):721-737(in Chinese with English abstract).
Xiao,X.C.,Li,T.D.,2000.Mechanism of Tectonic Evolution and Uplift of the Qinghai-Tibet Plateau.Guangdong Science and Technology Press,Guangzhou(in Chinese).
Yan,Z.,Wang,Z.Q.,Fu,C.L.,et al.,2018.Characteristics and Thematic Geological Mapping of Mélanges.Geological Bulletin of China,37(2):167-191(in Chinese with English abstract).
Zhang,J.,Deng,J.F.,Xiao,Q.H.,et al.,2012.New Advances in the Study of Ophiolites.Geological Bulletin of China,31(1):1-12(in Chinese with English abstract).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2016.Palaeogeographic Distribution and Tectonic Evolution of OPS in China.Earth Science Frontiers,23(6):24-30(in Chinese with English abstract).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2018.TectonicStratigraphic Division and Sedimentary Tectonic Evolution in China(in Chinese).
Zhang,K.X.,Yin,H.F.,Zhu,Y.H.,et al.,2001.Theory,Methodology and Practice of Geological Mapping in Mélange Terrains of Orogenic Belts:A Case Study of the East Kunlun Orogenic Belt.China University of Geosciences Press,Wuhan(in Chinese).
Zhang,W.Y.,1986.Tectonics of Land and Sea in China and Adjacent Areas.Science Press,Beijing,444-479(in Chinese).
鲍佩声,苏犁,王军,等,2015.雅鲁藏布江蛇绿岩.北京:地质出版社,227-233.
陈超,毛新武,胡正祥,等,2017.鄂北大洪山地区~817 Ma洋岛玄武岩的发现及意义.地质科技情报,36(6):22-31.
程裕淇,王鸿祯,2006.地质科学大辞典(基础学科卷).北京:地质出版社,794.
冯益民,张越,2018.大洋板块地层(OPS)简介及评述.地质通报,37(4):523-531.
胡正祥,毛新武,田望学,等,2015.扬子陆块北缘大洪山地区发现晋宁期造山带.中国地质调查,2(2):33-39.
黄汲清,陈炳蔚,1987.中国及邻区特提斯海的演化.北京:地质出版社,71-74.
孔令耀,毛新武,陈超,等,2017.扬子北缘大洪山地区中元古代打鼓石群碎屑锆石年代学及其地质意义.地球科学,42(4):485-501.
李四光,2016.天文·地质·古生物.北京:地质出版社,127-134.
李廷栋,1998.多金属结核.见:陈述彭,编,地球系统科学.北京:中国科学技术出版社,420.
李廷栋,2010.李廷栋文集(中卷).北京:地质出版社,1246.
李正祥,2015.华南大地构造演化综述:板块构造、地质事件与资源效应.北京:科学出版社,54-88.
莫杰,2004.海洋地学前缘.北京:海洋出版社.
潘桂棠,肖庆辉,2016.中国大地构造图(1∶2500 000)说明书.北京:地质出版社.
王希斌,鲍佩声,邓万明,等,1987.西藏蛇绿岩.北京:地质出版社.
肖庆辉,李廷栋,潘桂棠,等,2016.识别洋陆转换的岩石学思路---洋内弧与初始俯冲的识别.中国地质,43(3):721-737.
肖序常,李廷栋,2000.青藏高原的构造演化与隆升机制.广州:广东科技出版社.
闫臻,王宗起,付长垒,等,2018.混杂岩基本特征与专题地质填图.地质通报,37(2):167-191.
张进,邓晋福,肖庆辉,等,2012.蛇绿岩研究的最新进展.地质通报,31(1):1-12.
张克信,何卫红,徐亚东,等,2016.中国洋板块地层分布及构造演化.地学前缘,23(6):24-30.
张克信,何卫红,徐亚东,等,2018.中国构造-地层区划与沉积大地构造演化报告.
张克信,殷鸿福,朱云海,等,2001.造山带混杂岩区地质填图理论、方法与实践:以东昆仑造山带为例.武汉:中国地质大学出版社.
张文佑,1986.中国及邻区海陆大地构造.北京:科学出版社,444-479.
Bierlein,F.P.,Groves,D.I.,Cawood,P.A.,2009.Metallogeny of Accretionary Orogens-The Connection between Lithospheric Processes and Metal Endowment.Ore Geology Reviews,36:282-292.
Bierlein,F.P.,Groves,D.I.,Goldfarb,R.J.,et al.,2006.Lithospheric Controls on the Formation of Provinces Hosting Giant Orogenic Gold Deposits.Mineralium Deposita,40:874-887.
Chen,C.,Mao,X.W.,Hu,Z.X.,et al.,2017.Discovery of~817Ma Oceanic Island Basalts in the Dahongshan Region,Northern Hubei Province and Its Significance.Geological Science and Technology Information,36(6):22-31(in Chinese with English abstract).
Cheng,Y.Q.,Wang,H.Z.,2006.A Dictionary of Earth Science:Basic Sciences.Geological Publishing House,Beijing,794(in Chinese).
Dilek,Y.,Furnes,H.,2011.Ophiolite Genesis and Global Tectonics:Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere.Geological Society of America Bulletin,123(3-4):387-411.https://doi.org/10.1130/b30446.1
Dilek,Y.,Robinson,P.T.,2003.Ophiolites in Earth History.Geological Society,London,Special Publications,218:9-19.
Feng,Y.M.,Zhang,Y.,2018.Introduction and Commentary on Ocean Plate Stratigrapgy.Geological Bulletin of China,37(4):523-531(in Chinese with English abstract).
Herrington,R.J.,Brown,D.,2011.The Generation and Preservation of Mineral Deposits in Arc-Continent Collision Environments.Frontiers in Earth Sciences,(Chapter 6):145-159.https://doi.org/10.1007/978-3-540-88558-0
Hu,Z.X.,Mao,X.W.,Tian,W.X.,et al.,2015.Discovery of the Jinningian Orogenic Belt on the Northern Margin of Yangtze Craton in Mountain Dahong.Geological Survey of China,2(2):33-39(in Chinese with English abstract).
Huang,J.Q.,Chen,B.W.,1987.The Evolution of the Tethys in China and Adjacent Regions.Geological Publishing House,Beijing,71-74(in Chinese).
Hutchison,J.S.,Goldman,B.D.,1975.The Relationship between the Rat of Testosterone Infusion and Gonadotropin Secretion.Endocrinology,97(3):725-730.
Isozaki,Y.,Maruyama,S.,Furuoka,F.,1990.Accreted Oceanic Materials in Japan.Tectonophysics,181(1-4):179-205.https://doi.org/10.1016/0040-1951(90)90016-2
Kong,L.Y.,Mao,X.W.,Chen,C.,et al.,2017.Chronological Study on Detrital Zircons and Its Geological Significance from Mesoproterozoic Dagushi Group in the Dahongshan Area,North Margin of the Yangtze Block.Earth Science,42(4):485-501(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.039
Kusky,T.M.,Windley,B.F.,Safonova,I.,et al.,2013.Recognition of Ocean Plate Stratigraphy in Accretionary Orogens through Earth History:A Record of 3.8Billion Years of Sea Floor Spreading,Subduction,and Accretion.Gondwana Research,24(2):501-547.https://doi.org/10.1016/j.gr.2013.01.004
Li,S.G.,2016.Astronomy,Geology,Palaeontology.Geological Publishing House,Beijing,127-134(in Chinese).
Li,T.D.,1998.Polymetallic Nodules.In:Chen,S.P.,ed.,Earth System Science.China Science and Technology Press,Beijing,420(in Chinese).
Li,T.D.,2010.The Works of Li Tingdong.Geological Publishing House,Beijing,1246(in Chinese with English abstract).
Li,Z.X.,2015.Summary of Tectonic Evolution in South China:Plate Tectonics,Geological Events and Resource Effects.Science Publishing House,Beijing,54-88(in Chinese).
Maruyama,S.,Kawai,T.,Windley,B.F.,2010.Ocean Plate Stratigraphy and Its Imbrication in an Accretionary Orogen:The Mona Complex,Anglesey-Lleyn,Wales,UK.Geological Society,London,Special Publications,338(1):55-75.https://doi.org/10.1144/sp338.4
Mo,J.,2004.Frotiers on Marine Geoscience.China Ocean Press,Beijing(in Chinese).
Pan,G.T,Xiao,Q.H.,2016.Explanatory Note to the Tectonic Map of China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Safonova,I.,Biske,G.,Romer,R.L.,et al.,2016.Middle Paleozoic Mafic Magmatism and Ocean Plate Stratigraphy of the South Tianshan,Kyrgyzstan.Gondwana Research,30:236-256.https://doi.org/10.1016/j.gr.2015.03.006
Safonova,I.Y.,Santosh,M.,2014.Accretionary Complexes in the Asia-Pacific Region:Tracing Archives of Ocean Plate Stratigraphy and Tracking Mantle Plumes.Gondwana Research,25(1):126-158.https://doi.org/10.1016/j.gr.2012.10.008
Wakita,K.,Metcalfe,I.,2005.Ocean Plate Stratigraphy in East and Southeast Asia.Journal of Asian Earth Sciences,24(6):679-702.https://doi.org/10.1016/j.jseaes.2004.04.004
Wang,X.B.,Bao,P.S.,Deng,W.M.,et al.,1987.The Ophiolite in Tibet.Geological Publishing House,Beijing(in Chinese).
Xiao,Q.H.,Li,T.D.,Pan,G.T.,et al.,2016.Petrologic Ideas for Identification of Ocean-Continent Transition:Recognition of Intra-Oceanic Arc and Initial Subduction.Geology in China,43(3):721-737(in Chinese with English abstract).
Xiao,X.C.,Li,T.D.,2000.Mechanism of Tectonic Evolution and Uplift of the Qinghai-Tibet Plateau.Guangdong Science and Technology Press,Guangzhou(in Chinese).
Yan,Z.,Wang,Z.Q.,Fu,C.L.,et al.,2018.Characteristics and Thematic Geological Mapping of Mélanges.Geological Bulletin of China,37(2):167-191(in Chinese with English abstract).
Zhang,J.,Deng,J.F.,Xiao,Q.H.,et al.,2012.New Advances in the Study of Ophiolites.Geological Bulletin of China,31(1):1-12(in Chinese with English abstract).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2016.Palaeogeographic Distribution and Tectonic Evolution of OPS in China.Earth Science Frontiers,23(6):24-30(in Chinese with English abstract).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2018.TectonicStratigraphic Division and Sedimentary Tectonic Evolution in China(in Chinese).
Zhang,K.X.,Yin,H.F.,Zhu,Y.H.,et al.,2001.Theory,Methodology and Practice of Geological Mapping in Mélange Terrains of Orogenic Belts:A Case Study of the East Kunlun Orogenic Belt.China University of Geosciences Press,Wuhan(in Chinese).
Zhang,W.Y.,1986.Tectonics of Land and Sea in China and Adjacent Areas.Science Press,Beijing,444-479(in Chinese).
鲍佩声,苏犁,王军,等,2015.雅鲁藏布江蛇绿岩.北京:地质出版社,227-233.
陈超,毛新武,胡正祥,等,2017.鄂北大洪山地区~817 Ma洋岛玄武岩的发现及意义.地质科技情报,36(6):22-31.
程裕淇,王鸿祯,2006.地质科学大辞典(基础学科卷).北京:地质出版社,794.
冯益民,张越,2018.大洋板块地层(OPS)简介及评述.地质通报,37(4):523-531.
胡正祥,毛新武,田望学,等,2015.扬子陆块北缘大洪山地区发现晋宁期造山带.中国地质调查,2(2):33-39.
黄汲清,陈炳蔚,1987.中国及邻区特提斯海的演化.北京:地质出版社,71-74.
孔令耀,毛新武,陈超,等,2017.扬子北缘大洪山地区中元古代打鼓石群碎屑锆石年代学及其地质意义.地球科学,42(4):485-501.
李四光,2016.天文·地质·古生物.北京:地质出版社,127-134.
李廷栋,1998.多金属结核.见:陈述彭,编,地球系统科学.北京:中国科学技术出版社,420.
李廷栋,2010.李廷栋文集(中卷).北京:地质出版社,1246.
李正祥,2015.华南大地构造演化综述:板块构造、地质事件与资源效应.北京:科学出版社,54-88.
莫杰,2004.海洋地学前缘.北京:海洋出版社.
潘桂棠,肖庆辉,2016.中国大地构造图(1∶2500 000)说明书.北京:地质出版社.
王希斌,鲍佩声,邓万明,等,1987.西藏蛇绿岩.北京:地质出版社.
肖庆辉,李廷栋,潘桂棠,等,2016.识别洋陆转换的岩石学思路---洋内弧与初始俯冲的识别.中国地质,43(3):721-737.
肖序常,李廷栋,2000.青藏高原的构造演化与隆升机制.广州:广东科技出版社.
闫臻,王宗起,付长垒,等,2018.混杂岩基本特征与专题地质填图.地质通报,37(2):167-191.
张进,邓晋福,肖庆辉,等,2012.蛇绿岩研究的最新进展.地质通报,31(1):1-12.
张克信,何卫红,徐亚东,等,2016.中国洋板块地层分布及构造演化.地学前缘,23(6):24-30.
张克信,何卫红,徐亚东,等,2018.中国构造-地层区划与沉积大地构造演化报告.
张克信,殷鸿福,朱云海,等,2001.造山带混杂岩区地质填图理论、方法与实践:以东昆仑造山带为例.武汉:中国地质大学出版社.
张文佑,1986.中国及邻区海陆大地构造.北京:科学出版社,444-479.
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