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《Journal of Central South University(Science and Technology)》 2015-02
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Geochemical characteristics of intrusion in Guangxi Dachang ore field and its ore-forming significance

CHENG Yongsheng;Key Laboratory of Metallogenic Prediction of Nonferrous Metals,Ministry of Education, Central South University;School of Geosciences and Info-Physics, Central South University;State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry,Chinese Academy of Sciences;  
Based on the analysis of the major elements, trace elements and rare earth elements, the petrogenesis and evolution of intrusion and the tectonic environment of diagenesis and mineralization were discussed. The results show that w(LREE), w(HREE) and w(ΣREE) are(28.25-144.85)×10-6,(4.28-14.75)×10-6 and(32.53-159.6)×10-6, respectively. The range of w(LREE)/w(HREE), δw(Eu), δw(Ce), w(Gd)/w(Yb) w(Sm)/w(Nd), w(Eu)/w(Sm) and w(La)/w(Sm) varies from6.22 to 12.33,0.29 to 0.71,0.94 to 0.97,1.61 to 2.31,0.16 to 0.23,0.10 to 0.24 and 6.06 to 9.41,respectively. The intrusions are mainly of aluminum-strongly peraluminous series, characterized by silica poor, relative stable content of the large ion lithophile elements, high content of the inactive elements, low content of the high field strength elements, high concentration of LREE, depleted in HREE and high fractionation for REE. Chondrite-normalized REE patterns with good consistency suggest maybe the same or similar magma source and evolutionary history. The intrusions, whose evolutions are affected by the crust-mantle which supplied the material source, belong to the product of the crust-mantle interaction.The rock may be the result of the partial melting in means of the crust and mantle mixed in the period of collision orogeny and intra-plate, special in the conversion period both of them, in the tensile tectonic environment.
【Fund】: 国家自然科学基金资助项目(41202051);; 湖湘青年科技创新创业平台培养对象人才基金项目(湘科人字[2014]76号);; 中国博士后科学基金特别资助项目(2014T70886);中国博士后科学基金面上资助项目(2012M521721)~~
【CateGory Index】: P613
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【Citations】
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Chinese Journal Full-text Database 10 Hits
1 Zhao Jiao;Zhang Chengli;Liu Xinyu;Guo Xiaojun;State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University;No.5 Gold Geological Party of Chinese Armed Police Force;;Protolith age and geochemical characteristics of meta-basic volcanic rocks from Lüliang Group in the Lüliang complex and its tectonic setting[J];地质科学;2017-04
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3 Ziye Wang;Renguang Zuo;Zhenjie Zhang;State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences;School of the Earth Sciences and Resources, China University of Geosciences;;Spatial Analysis of Fe Deposits in Fujian Province, China: Implications for Mineral Exploration[J];Journal of Earth Science;2015-06
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5 Qin Ya;Zhang Qingwei;Kang Zhiqiang;Li Saisai;Feng Zuohai;Yang Qijun;Pang Baocheng;Bai Ling'an;Xie Yongbin;Ye Ming;Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration,Guilin University of Technology;Guangxi Zhuang Autonomous Region Geological Environmental Monitoring Station;;Geochronological Framework of Granitoids in Dayaoshan Metallogenic Belt,Eastern Guangxi Province[J];吉林大学学报(地球科学版);2015-06
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