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《Acta Geologica Sinica》 2008-09
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Re-Os Isotope Study of Sulfide and Olivine Pyroxenite in the Limahe Nickle Deposit,Sichuan Province

TAO Yan1), HU Ruizhong1), QU Wenjun2), DU Andao2) 1) State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550002; 2) Chinese Academy of Geological Sciences, National Research Center for Geo Analysis, Beijing, 100037  
The Limahe nickel deposit is one of the important PGE-poor Ni-Cu deposit in the Emeishan Large Igneous Province. This paper mainly analyzes Re-Os isotopic composition of various ore and rocks from the Limahe nickel deposit, discusses source magma, genesis of suphide, ore-forming mechanism and Re-Os isochron. The results show that different rock and rock types of the Limahe deposit are of different initial Os isotopic compositions. The differences of initial Os isotopic composition between sulfide-rich veinlet ores and their ssextracted sulfide are small and their isochron of 265±35 Ma is agreement to the zircon SHRIMP age of 263±3 Ma from the rock. Initial radiogenic Os concentrations between sulfide-poor ore and rock are distinctly different, and its isochron age is larger than metallogenic age. The analysis shows that heterogeneity of initial Os isotopic composition in the ore samples is attributed to the mixture of sulfide melt containing high radiogenic 187Os and silicate melt containing low radiogeneic 187Os at a different proportion. Mixed modeling suggests that the ore samples containing more than 30 % of sulfide have similar initial 187Os/188Os ratios, whilst the samples containing less than 30 % of sulfide have big difference in the initial 187Os/188Os depending on the contents of sulfide, providing a possible explanation for several sets of Re-Os isochron ages of the magmatic sulfide deposits. Radigenetic ore-forming rock samples with least abundance of 187Os has a γOs(t=260Ma) value of 5 and Cu/Pd ratio of 7000, indicating that they were the products of original magmatic crystallization without any crustal contamination and sulfide exsolution. It was estimated that the Os content in primary magma is about 1×10-9, suggesting a picritic magma in origin. Re/Os ratio of sulfide in the ores is higher than those of any ore-hosted peridotite, with γOs(t=260Ma) up to 110. Comprehensive study reveals that the Limahe deposit originated from a daughter magma which exsolved from deep magma. Model analysis indicates that sulfide in the deposit originated from two exsolution of primary magma, correspondingly, ore-forming magma had also experienced two contaminations in the lower and upper crusts in proportion of about 7%.
【Fund】: 国家自然科学基金(编号40773033 40572062);; 中国科学院重要方向项目(编号KZCX2-YW-111)资助的成果
【CateGory Index】: P597;P618.63
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3 GAO Yong-bao 1,2),LI Wen-yuan 1),ZHANG Zhao-wei 1,2),LI Chao 3),ZHOU Li-min 3),GUO Zhou-ping 1),ZHANG Jiang-wei 1),LI Kan 1),QIAN Bing 1),WANG Ya-lei 1),TAN Wen-juan 1) 1) Xi'an Institute of Geology and Mineral Resources,Xi'an,Shaanxi 710054;2) College of Earth Sciences and Land Resources,Chang'an University,Xi'an,Shaanxi 710054;3) National Research Center of Geoanalysis,Beijing 100037;Re-Os Isotopic Analysis of the Yulonggou Cu-Ni Sulfide Deposit in the South Qilian Mountain[J];Acta Geoscientica Sinica;2012-06
4 BAI Junhao;HUANG Zhilong;ZHU Dan;YAN Zaifei;ZHOU Jiaxi;State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences;Henan Institute of Geological Survey;Graduate University of Chinese Academy of Sciences;;Isotopic Compositions of Sulfur in the Jinshachang Lead–Zinc Deposit, Yunnan, China, and its Implication on the Formation of Sulfur-Bearing Minerals[J];地质学报(英文版);2013-05
5 BAI Jun-hao1,2,HUANG Zhi-long1,ZHU Dan1,YAN Zai-fei1,LUO Tai-yi1,ZHOU Jia-xi1(1.State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China);Characteristics of Sulfur Isotope Geochemistry of Jinshachang Pb-Zn Deposit in Yunnan Province, China[J];Acta Mineralogica Sinica;2013-02
6 CHEN Ci-yun,WEN Shu-ming,FENG Qi-cheng,ZHAO He-fei,WANG Yi-jie,LV Chao(Kunming University of Science and Technology,Kunming 650093,China);Comprehensive Utilization Status of Low Grade and Refractory Platinum-palladium Ores from Jinbaoshan of Yunnan[J];Conservation and Utilization of Mineral Resources;2013-01
7 LIU Jun PENG Xiu-hong HUANG Shi-zong XIANG Zhi-lei(1-Department of Geochemistry,Chengdu University of Technology,Chengdu 610059;2-No.403 Geological Team,BGEEMRSP,Emeishan,Sichuan 614200);Geochemical Characteristics of Pegmatite from Baima,Miyi,Sichuan[J];Acta Geologica Sichuan;2013-02
8 XIA Fang1,CHAI Feng-mei1,CHEN Bin1,2,LU Hong-fei3 and YAN Yu-pu4(1.Xinjiang Key Laboratory for Geodynamic Processes and Metallogenic Prognosis of the Central Asian Orogenic Belt,Urumqi 830049,China;2.School of Earth and Space Sciences,Peking University,Beijing 100871,China;3.No.6 Geological Party,Xinjiang Bureau of Geology and Mineral Resources,Hami 839000,China;4.Tuha Oilfield Exploration & Development Research Institute,Hami 839009,China);Geochemical characteristics of platinum group elements and Re-Os isotopes of the Hongshishan Cu-Ni sulfide-bearing mafic-ultramafic intrusion in Beishan block of Xinjiang and their metallogenic significance[J];Acta Petrologica Et Mineralogica;2012-01
9 LI YongSheng and ZHANG ZhaoChong** State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China;Application of energy-constrained assimilation-fractional crystallization(EC-AFC) model for ultramafic magmatic systems:A case study of the Limahe intrusion associated with Cu-Ni sulfide ores,Sichuan Province[J];Acta Petrologica Sinica;2011-10
10 CHEN Da1,LIU Yi2(1.Institute of Geological and Mineral Resource Exploration,Guizhou Non-ferrous Metals and Nuclear Geological Exploration Bureau,Guiyang 550005;2.Guizhou Academy of Geological Survey,Guiyang 550004);Discussion on the relationships between Emeishan basalt and Pb-Zn mineralization[J];Mineral Exploration;2012-04
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 SONG Xie-yan~(1,2), CAO Zhi-min~3, LUO Fu-xun~4, ZHU Ting-guo~4, LI You-guo~1, CHEN Jia-zhong~4 (1.College of Applied Nuclear Technology and Automation Engineering, Chengdu University of Technology, China; 2.Department of Earth Sciences, The University of Hong Kong, China; 3.Ocean University of China; 4.The 402 Geological Unit, Geology and Mineral Bureau of Sichuan, China);Origin of Yangliuping Ni-Cu-PGE sulfide deposit in Danba, Sichuan[J];Journal of Chengdu University of Technology(Science & Technology Edition);2004-03
2 HUANG Zhi-long 1 ,GUAN Tao 1,2 ,XIE Li-hua 1 and XU De-ru 1 (1.Institute of Geochemistry,Chinese Academy of Sciences,Guiyang550002,China;2.Graduate School of the Chinese Academy of Sciences,Beijin g100039,China;3.Guangzhou Institute of Geochemistr y,Chinese Academy of Sciences,Guangzhou510640,China);PETROLOGICAL MIXING CALCULATION AND ITS APPLICATION TO MAGMA FRACTIONAL CRYSTALLIZATION——A Case Study of Iamprophyres in Baima zhai Nickel Deposit,Yunnan Province[J];Geotectonica Et Metallogenia;2003-03
3 WANG Ruiting~(1,2), MAO Jingwen~(1,3), HE Ying~4, WANG Dongsheng~2 and TANG Zhongli~5 (1. Faculty of Geosciences and Resources, China University of Geosciences, Beijing 100083, China; 2. Bureau of Geological Exploration for Nonferrous Metals in Northwest China, Xi'an, SX 710054, China; 3. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; 4. Department of Geology, Northwest University, (Xi'an,) SX 710069, China; 5. Faculty of Geosciences and Resources, Chang'an University, (Xi'an), SX 710054, China);GEOCHEMICAL CHARACTERISTICS OF PLATINUM GROUP ELEMENTS IN JINCHUAN SUPER-LARGE SULFIDE COPPER- NICKEL DEPOSIT, JINCHANG CITY, GANSU PROVINCE, CHINA[J];Geotectonica Et Metallogenia;2004-03
4 Mei Hou-chun;THE RELATIONSHIP BETWEEN THE PETROCHEMICAL CHARACTERISTICS OF TWO TRAP SERIES IN SOUTHWESTERN CHINA AND RELATED IRON AND NICKEL MINERALIZATIONS[J];Geochimica;1973-04
5 Luo Yaonan(No. 106 Geological Team, Geological Bureau, Sichuan Province);THE CHARACTERISTICS OF Ti-CHROMITE MINERALIZATION IN XIN JIE LAYERED ULTRAMAFIC-MAFIC INTRUSION IN PANZIHUA AREA, CHINA[J];Geochimica;1981-01
6 Zhang Chengjiang; Wang Yunliang; Li Xiaoling; Xiu Shuzhi;Huang Yongjian (Chengdu Institute of Technology, Chengdu 610059)(Institute of High Energy Physics, Chinese Academy of Sciences, Beijing 100080);GEOCHEMISTRY OF PLATINUM GROUP ELEMENTS IN MAFIC-ULTRAMAFIC ROCKS FROM THE XINJIE INTRUSION[J];Geochimica;1998-05
7 XU Yi-Gang1, CHUNG Sun-Lin2 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. Department of Geology, National Taiwan University, Taibei, China);The Emeishan Large Igneous Province: Evidence for mantle plume activity and melting conditions[J];Geochimica;2001-01
8 Ran Hongyan; Xiao Senhong (Guangzhou Branch, Institute of Geochemistry, Academia Sinica, Guangzkou 510640);TRACEELEMENT ABUNDANCES AND TECTONIC ENVI-RONMENT OF THE HOST INTRUSION OF KALATONGKE Cu-Ni DEPOSIT[J];GEOCHIMICA;1994-04
9 Gao Huaizhong (China University of Geosciences, Wuhan 430074);GEOLOGICAL CHARACTERISTICS OF NO.1 BASIC ULTRABASIC INTRUSIVE BODY AND ITS ORE POTENTIALITY,POBEI,XINJIANG[J];;1992-04
10 LI XIAO-LIN; CHAI ZHI-FANG; MAO XUE-YING (The Laboratory of Nuclear Analytical Techniques, InStitute of high Energy Physics,Chinese Academy of Sciences, Beijing 100080, China);STUDY OF GEOCHEMICAL TRACING OF PLATINUM GROUP ELEMENTS: THE GEOCHEMICAL CHARACTERISTICS OF PLATINUM GROUP ELEMETS IN XINJIE LAYERED INTRUSION, SICHUAN PROVINCE[J];Chinese Journal of Geophysics;1998-S1
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