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《Journal of Jilin University(Earth Science Edition)》 2011-01
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On Failing of the Magmatic Hydrothermal Metallogenic Theory:the Causes and the New Departure

LUO Zhao-hua1,LU Xin-xiang2,LIU Cui1,LI De-dong1,YANG Zong-feng1,WEN Si-bo1 1.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China 2.Scientific Academy of Land and Resources of Henan Province,Zhengzhou 450053,China  
The current magmatic hydrothermal metallogenic theory(MHMT) assumes that the ore-bearing fluids are produced from the magma by differentiation,especially,by fractional crystallization.Attending to the close relation between the giant and super giant deposits and the minor intrusions,and to that a minor intrusion can not satisfies the mass balance,the endorsers further emphasize that there is a large magma chamber beneath the minor intrusion.Such interpretations are contrary to the observations in the ore fields and the theoretical deductions:(1) There are commonly many minerals which have greater densities than the host magma and melano-microgranular enclaves in the ore-bearing porphyries.This means there was not fractional crystallization in both the minor intrusion and the possible deep magma chamber.(2) There is not any evidence to suggest that the fluid produced by magmatic differentiation will be in action only then when the melt is consolidated,because the fluid is more active than the melt.(3) The wide compositional spectrum dike swarms are widespread seen in the ore fields.It is suggested that there was not syn-metallogenic large deep chamber beneath the minor intrusion.Therefore,the MHMT found itself in a tight corner not only due to the mass balance.It is necessary to consider new mechanisms related to metallogenesis of the endogenic mineral deposits.The root-cause induced the MHMT to failed is that the ore-forming processes are considered as equilibrium linear processes taken place in the ideal systems.The ore-forming system is actually a complex dynamic system and the mineralization is a non-equilibrium and non-linear process.In other words,the ore-forming system and the mineralization are understood incorrectly in the prevalent MHMT.At the modern level of sciences,its failing is inevitable.Then,it is necessary to construct a new theory.Based on the cardinal principles of science of complexity,Luo,et al.(2007,2009) considered the melt and the ore-bearing fluid as two subsystems in the metallogenic system.Their strong interactions and the environmental constraints trigger the dramatic development in the metallogenic system.They further provide a new framework model named as the metallogenic theory by transmagmatic fluids(TMFT).The theory can not only explain more mineralizing phenomena than the MHMT can do,but it also has ability to deduce potential and practical indicators for the metallogenic prognosis.Therefore,it is possible that the TMFT will become to the new departure of the metallogenesis of the magma-related deposits.
【Fund】: 中俄合作基金项目(40911120079 RFBR-GFEN08-05-92224);; 有色金属矿产地质调查中心危机矿山勘查理论项目(200699105-4);; 中国地质调查局地质调查工作项目(1212010911028);; 天津华北地质勘查总院科研项目(KY2008-2);; 国家自然科学基金项目(90814007)
【CateGory Index】: P611
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10 ZHANG Qi;Institute of Geology and Geophysics,Chinese Academy of Sciences;;DISCUSSION ON “SMALL INTRUSIONS ASSOCIATE WITH LARGE DEPOSITS” AND “LARGE INTRUSIONS ARE NOT MINERALIZATION”[J];Gansu Geology;2013-04
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1 ZHANG Qi~1,JIN Wei-jun~1,LI Cheng-dong~2,JIAO Shou-tao~1 (1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2.Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China);Identification and implication of magma thermal field in the geothermal field[A];[C];2014
2 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);PROBLEM OF ORE-BEARING ROCK BODY AND ORE-FORMINGMOTHER ROCK BODY[A];[C];2014
3 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);DISCUSSION ON THE SITE OF THE BEST MINERALIZATION OF MAGMATIC HYDROTHERMAL DEPOSITS[A];[C];2014
4 LUO Zhao-hua;SU Shang-guo;LIU Cui;State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences;;Scale Effects of the Magma-related Metallogenic Systems[A];[C];2014
5 YAN Hai-qing;HE Bao-lin;LIU Qiao-feng;JIA Hui-min;LI Fei;School of Earth Science and Resources,Chang'an University;No.1 Institute of Geological and Mineral Resources Survey,Henan Provincial Bureau of Geo-exploration and Mineral Development;No.5 Gold Geological Party of Chinese People's Armed Police Force;;Characteristics of Magmatic Geochronology and Geochemistry of Dashui Gold Deposit in West Qinling[A];[C];2014
6 ZHANG Qi;JIN WeiJun;LI ChengDong;JIAO ShouTao;Institute of Geology and Geophysics,Chinese Academy of Sciences;Tianjin Institute of Geology and Mineral Resources,China Geological Survey;;Magma-thermal field:Its basic characteristics,and differences with geothermal field[A];[C];2015
7 ZHANG Qi;JIN Wei-jun;LI Cheng-dong;JIAO Shou-tao;Institute of Geology and Geophysics,Chinese Academy of Sciences;Tianjin Institute of Geology and Mineral Resources,China Geological Survey;;THE THEORY OF "MAGMA THERMAL FIELD" AND ITS METALLOGENIC SIGNIFICANCE[A];[C];2015
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2 ZHANG Shuangtao 1),2) WU Tairan 1),2) XU Xuan 1),2) J.BYAMBA 3) A.AMARJARGAL 3) WANG Shiqi 2) LI Zhongquan 2) ( 1)Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education,Peking University, Beijing 100871; 2) School of Earth and Space Sciences, Peking University, Beijing 100871; 3) Faculty of Earth Science, National University of Mongolia, Ulaanbaatar, Mongolia);The Significance of Discovery of Early Cretaceous Shoshonite in Central Inner Mongolia[J];Acta Scicentiarum Naturalum Universitis Pekinesis;2005-02
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7 WANG Dong-yan~(1),XU Wen-liang~(1),LAN Xiang~(2),WANG Qing-hai~(1) (1.College of Earth Sciences, Jilin University, Changchun130061,China; 2.Department of Earth Science, Zhejiang University, Hangzhou310027,China);Petrogenesis of pyroxenite xenoliths in Mesozoic gabbro-diorite from western Shandong Province, China[J];Journal of Jiling University (Earth Science Edition);2004-02
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9 SUN Lin-hua1,2,WANG Yue-jun1,FAN Wei-ming1,ZI Jian-wei11.Key Laboratory of Isotope Geochronology and Geochemistry,Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou 510640,China2.Graduate University,Chinese Academy of Sciences,Beijing 100039,China;A Further Discussion of the Petrogenesis and Tectonic Implication of the Mazhashan Syenites in the Bachu Area[J];Journal of Jilin University(Earth Science Edition);2008-01
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