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《Acta Geologica Sinica》 2008-09
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Petrologic Characteristics of the Granites and Greisens and Muscovite ~(40)Ar/~(39)Ar Dating in the Taoxikeng Tungsten Polymetallic Deposit,Southern Jiangxi Province

GUO Chunli1), LIN Zhiyong2), WANG Denghong1), CHEN Wen3), ZHANG Yan3), FENG Chengyou1), CHEN Zhenghui1), ZENG Zailin4), CAI Ruqing5)1) Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037; 2) China Geological Survey, Beijing,100011; 3) Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037; 4) Gannan Geological Survey Party of Jiangxi Province, Ganzhou, 341000; 5) China University of Geosciences, Beijing, 100083  
The Taoxikeng tungsten-polymetallic deposit, Congyi County, Southern Jiangxi Province, in the central Nanling region, South China, consists of vein-type ore bodies hosted in Cambrian to Jurassic strata, and is closely related to Mesozoic granitic intrusions. Wolframite is the dominant ore minerals intergrown with gangue minerals of quartz, feldspar, phlogopite, and muscovite. We have carried out muscovite 40Ar/39Ar dating to better understand the time and genesis of mineralization. Muscovite 40Ar/39Ar dating of five greisen samples from different intermediate sections yielded well-defined 40Ar/39Ar plateau ages of 152.7±1.5Ma, 153.4±1.3Ma and 155.0±1.4 Ma. Compared with known other datings, we found that the formation of granite and mineralization are at the same time. Based on the analytical data and experimentally geochemical data available, it is pointed out that the tetrad effects of REE in the granites and greisens are produced in the melt-fluid system. Intense fractional crystallization of granitic melt (containing REE accessories) and its interaction with volatile-rich (F, Cl) fluid are the major factors leading to the tetrad effects of REE. Our new data, when combined with published geochronological results from other major deposits in Nanling region, suggest that large-scale W, Sn, Mo, Bi, Nb, Ta, Pb, Zn mineralization occurred throughout the central and eastern Nanling region at 160~150Ma, which indicates a geodynamic setting of crustal extension during the transformation of tectonic regimes during the Mid-Late Jurassic.
【Fund】: 国土资源大调查计划项目(编号1212010633903);; 中央级公益性科研院所基本科研业务专项资金(编号K0703);; 国家重点基础研究项目(编号2007CB411070507);; 国家自然科学基金(编号40772063)资助的成果
【CateGory Index】: P618.2;P597
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3 ZOU Xian-wu1,CUI Sen1,QU Wen-jun2,BAI Yun-shan1,CHEN Xi-qing1(1.Yichang Institute of Geology and Mineral Resources,Yichang 443003,Hubei,China;2.National Research Center of Geoanalysis,Beijing 100037,China);Re-Os isotope dating of the Liguifu tungsten-tin polymetallic deposit in Dupangling area,Guangxi[J];Geology in China;2009-04
4 ZHANG Hai1,2,FANG Wei-xuan2,Zhang Guishan3,GAN Feng-wei2,WEI Ning1,2,Guo Yu-qian2(1.School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;2.Beijing Institute of Geology for Mineral Resources,Beijing 100012,China;3.College of Earth Sciences and Resources,Chang'an University,Xi'an 710054,Shaanxi,China);Facies sequence reestablishment and metallogenic analysis of Middle Triassic Anisian meta-volcanic rocks in the Kafang ore district,Gejiu,Yunnan[J];Geology in China;2009-06
5 LI Yan-jun1,WEI Jun-hao1,WU Gang1,TAN Jun1,JIANG Yong-jian1,FU Le-bing1,QU Wen-jun2,LOU Wang-ping3,XIE Chang-cai3 1.Faculty of Earth Resources,China University of Geosciences,Wuhan 430074,China 2.National Research Center of Geoanalysis,Beijing 100037,China 3.No.7 Geological Team of Zhejiang Province,Lishui 323000,China;Re-Os Dating of Molybdenite from the Maoduan Lead-Zinc Polymetallic Deposit in Southwestern Zhejiang Province and Its Geological Significance[J];Earth Science(Journal of China University of Geosciences);2011-02
6 Dai Yanpei1,Yu Xinqi1,Wu Ganguo1,Li Chunlin1,Qiu Junting1,Zhang Jiajing2,Luo Ping1,2 1.School of the Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China 2.Northeastern Jiangxi Geological Party of Jiangxi Province,Shangrao 334000,China;Characteristics of sulfide minerals,genetic type and metallogenic epoch of the Caijiaping lead-zinc deposit,North Wuyi Area,Jiangxi Province.[J];Earth Science Frontiers;2011-02
7 XIAO Guang-ling1,SUN Xiao-yan2,WANG Qi3,LIU Guo-chun3,YU Hai-tai3,LI Yan-jun1,PAN Jin-bo4(1.Faculty of Earth Resources,China University of Geosciences,Wuhan 430074,China;2.Lingbao Gold Limited Company,Lingbao Henan 472532,China;3.Chifeng Geological Prospecting Institute,Chifeng Inner Mongolia 024005,China;4.No.11 Geological Team of Zhejiang Bureau of Geology and Mineral Resource,Wenzhou Zhejiang 325006,China);Geology,Mineralization Age and Genesis of the Shipingchuan Molybdenum Deposit,Southeastern Zhejiang Province[J];Geological Science and Technology Information;2010-01
8 ZHOU Zhen-hua1,Lü Lin-su2,WANG Ai-shun3(1.MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of MineralResources,Chinese Academy of Geological Sciences,Beijing 100037,China;2.The Geological Museum of China,Beijing 100034,China;3.Geological SurveyInstitute of Inner Mongolia,Hohhot 010020,China);Deep Source Characteristics and Tectonic-Magmatic Evolution of Granites in the Huanggang Sn-Fe Deposit,Inner Mongolia:Constraint from Sr-Nd-Pb-Hf Multiple Isotopes[J];Geological Science and Technology Information;2011-01
9 MAO Jingwen1), XIE Guiqing1), CHENG Yanbo2), CHEN Yuchuan1) 1) MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, 100037; 2) Faculty of Earth Sciences, China University of Geosciences, Beijing, 100083;Mineral Deposit Models of Mesozoic Ore Deposits in South China[J];Geological Review;2009-03
10 WANG Yanbin1), WANG Denghong2), HAN Juan1), LEI Zeheng3), CHEN Zhenghui2), QU Wenjun4), XU Yiming3),ZI Baizhong3), Wang Qingli5)1) Beijing SHRIMP Lab, Institute of Geology, Chinese Academy of Geological Sciences, Beijing,100037;2) Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing,100037;3) Southern Hunan Institute of Geology and Survey , Chenzhou,Hunan,423000;4) National Research Center of Geoanalysis , Beijing ,100037;5) College of Enviroment and Planning, Henan University, Kaifeng, Henan, 475001,China;U-Pb Dating and Hf Isotopic Characteristics of Zircons and Re-Os Dating of Molybdenite from Gao'aobei Tungsten—molybdenum Deposit,Southern Hunan Province[J];Geological Review;2010-06
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6 FU Jianming~(1,2), MA Changqian~1, XIE Caifu~2, ZHANG Yeming~2 and PENG Songbai~2 (1. Faculty of Earth Sciences, China University of Geosciences, Wuhan, HB 430074, China; 2. Yichang Institute of Geology and Mineral Resources, Yichang, HB 443003, China);SHRIMP U-Pb ZIRCON DATING OF THE JIUYISHAN COMPOSITE GRANITE IN HUNAN AND ITS GEOLOGICAL SIGNIFICANCE[J];Geotectonica Et Metallogenia;2004-04
7 HUANG Ge-fei 1 ,ZENG Qin-wang 2 ,WEI Shao-liu 1 ,XU Yi-ming 1 ,HOU Mao-song 1 and KANG Wei-qing 1(1.Xiangnan Institute of Mineral Resources and Survey,Hunan Institute of Geological Survey,Chenzhou423000,Hunan,China;2.Huna;Geological characteristics and ore-controlling factors of the Furong orefield,Qitianling,Hunan[J];Chinese Geology;2001-10
8 WEI Shao-liu,ZENG Qin-wang,XU Yi-ming,LAN Xiao-ming,KANG Wei-qing,LIAO Xing-yu (Hunan Institute of Geological Survey,Changsha410011,Hunan,China);Characteristics and ore prospects of tin deposits in the Qitianling area,Hunan[J];Chinese Geology;2002-01
9 ZHANG Bang-tong,CHEN Pei-rong,KONG Xing-gong (Department of Earth Sciences and State Key Laboratory for Mineral Deposit s Research,Nanjing University,Nanjing210093,China);Rb-Sr chronology of bimodal volcanic rocks of the Yutian Group in the Linjiang basin,southern Jiangxi[J];Chinese Geology;2002-04
10 FU Jian-ming 1,2 ,MA Chang-qian 1 ,XIE Cai-fu 2 ,ZHANG Ye-ming 2 ,PENG Song-bai 2(1.China University of Geosciences,Wuhan430074,Hubei,China;2.Yichang Institute of Geology and Mineral Resources,Yichang443003,Hubei,China);Zircon SHRIMP dating of the Cailing granite on the eastern margin of the Qitianling granite,Hunan,South China,and its significance[J];Chinese Geology;2004-01
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