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《Journal of Jilin University(Earth Science Edition)》 2006-04
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Mantle Fluid's Action in the Processes of Petrogenesis of Alkalic Porphyry and Associated Mineralizations,Western Yunnan,China-Constraint of Geochronology and Isotope Geochemistry

LIU Xian-fan,SONG Xiang-feng,LU Qiu-xia,TAO Zhuan,LONG Xun-rongCollege of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China  
There are well-developed alkali-rich porphyry polymetallic deposits in the eastern Jinshajiang-Ailaoshan fault,western Yunnan.The alkali-rich porphyries in the region have been disco-(vered) containing deep xenoliths.The studies on the geochronology for deep xenoliths,their host alkalic porphyries and mineralizing quartz viens show that the diagenetic age of the deep xenoliths are older than that of their host alkalic porphyry,and the alkalic porphyry's diagenesis and associated mineralization are almost same in age.Combined with the studies of Pb-Si-Sr-Nd(isotopic) geochemistry,it is indicated that during the period of alkalic magma diagenisis the alkalic porphyry and its country rocks were suffered metasomatic alteration by the silicon-rich mineralizing fluids which were contaminated with crustal rocks,meanwhile,the ore deposits were formed.The mineralizing process of the silicon-rich fluids is essentially a continuation of the mantle fluid metasomatism during mineralizing processes in the crust.The mineral crystalline age(116.0 Ma) of the mantle fluid metasomatism and the age(51.2 Ma) of the silicon-rich mineralizing fluid suggest that the mantle fluid had been active through the whole processe of the alkalic magma diagenism and associated mineralization.The mantle fluid resulted in the concentrations of Si,Al,Na,K,Si-incompatible elements and ore elements,and the transition of Sr-Nd(isotopic) geochemistry from depleted mantle to enriched mantle,and the high temperature mineralization in the porphyry and the low temperature mineralization in the country rocks.The action of the mantle fluid is not only an internal constraint to wide spread Cenozoic mineralization but also an important geochemical background for the formation of large and super-large deposits in the western Yunnan,China.
【Fund】: 国家自然科学基金项目(40473027);; 中国地质大学地质过程与矿产资源国家重点实验室基金(GPMR0509)
【CateGory Index】: P611
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Chinese Journal Full-text Database 10 Hits
1 Zhang Zhilan Zhang .Shufa Yuan Haihua He Dalun;AN ISOTOPE GEOLOGY AND ORIGIN STUDY OF THE JINCHANG GOLD DEPOSIT,MOJIANG, YUNNAN[J];;1987-04
2 XIE Rongju;PENG Shenglin(Dept. of Geology, Cenral South University of Technology, Changsha 410083);K_2O CONTENT, K-METASOMATISM OF ROCK AND METALLOGENESIS[J];GEOTECTONICA ET METALLOGENIA;1998-03
3 ZHENG Jianpingn;LU Fengxiag;ZHAO Lei;WANG Baixuan;MAO Wenqing;SONG Genhe;(China University of Geosciences, Wuhan 430074)(The Laboratory of Crust-Mantle Constitution Recycling and Dynamics,Wuhan 430074)(China University of Geosciences,Beijing 100029)(The G;FLUIDS AND THEIR ROLES ON THE MANTLE EVOLUTION FROM THE PALAEOZOIC KIMBERLITES AND DIAMONDS IN NORTH CHINA PLATFORM[J];GEOTECTONICA ET METALLOGENIA;1996-02
4 Liu Xiaochun (Laboratory of Ore Deposite Geochemistry, Institute of Geochemistry, Academia Sinica, Guiyang 550002);ORIGIN OF ECLOGITE-GNEISS COMPLEXES FROM DABIE MOUNTAINS[J];GEOCHIMICA;1994-04
5 Can Ronglong,Zhu Shouhua(Guangzhou Institute of Geochemistry, Academia Sinica,Guangzhou 510640);THE MANTLE FLUID AND METALLOGENY[J];ADVENCE IN EARTH SCIENCES;1995-04
6 Sun Fengyue(Changchun College of Geology,Changchun,130026)Shi Zhunli(China University of Geosciences, Beijing, 1 00083);ON THE MANTLE-DERIVED C-H-O FLUID SYSTEM AND ITS SIGNIFICANCE TO SOME GEOLOGIC PROCESSES WITHIN CONTINENTAL PLATE[J];EARTH SCIENCE FRONTIERS;1995-02
7 Du Letian(Geological Research Institute of National Nuclear Cooperation,Beijing, 100029);THE RELATIONSHIP BETWEEN CRUST FLUIDS AND MANTLE FLUIDS[J];EARTH SCIENCE FRONTIERS;1996-04
8 Hu Zhengguo ( Xian College of Geology );A REVIEW ON EXPERIMENTAL STUDY OF THE FORMATION OF HYDROTHERMAL GOLD DEPOSIT[J];Geological Science and Technology Information;1989-04
9 Cai Xinpin (Institute of Geology Chinese Academy of Science,Beijing);DISCOVERY OF DEEP-DERIVED XENOLITHS IN CENOZOIC ALKALI-RICH PROPHRIES ALONG THE MARGIN OF THE YANGTZE PLATFORM AND ITS SIGNIFICANCE[J];Chinese Journal of Geology(Scientia Geologica Sinica);1992-02
10 Deng Wanming\ Huang Xuan\ Zhong Dalai (Institute of Geol. Chinese Academy of Sciences, Beijing\ 100029);PETROLOGICAL CHARACTERISTICS AND GENESIS OF CENOZOIC ALKALI RICH PORPHYRY IN WEST YUNNAN, CHINA[J];;1998-04
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