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《Mineral Deposits》 2010-01
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Metallogenic characteristics and formation mechanism of Zhaishang gold deposit,southern Gansu Province

LIU JiaJun1,MAO GuangJian1,WU ShengHua1,WANG JianPing1,MA XingHua2,LI LiXing3,LIU GuangZhi4,LIAO YanFu4 and ZHENG WeiJun4(1 State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China; 2 Department of Geology,Peking University,Beijing 100871,China; 3 Institute of Mineral Resources,Chinese Academy of Geolo-gical Sciences,Beijing 100037,China; 4 No. 5 Gold Geological Party of Chinese Armed Police Force,Xi'an 710100,Shanxi,China)  
Located in the western part of the Min-Li metallogenic belt within the West Qinling Mountains,the Zhaishang gold deposit is a large Carlin-type disseminated gold deposit discovered in recent years. The ore deposit occurs in the slightly metamorphosed Middle Devonian and Lower Permian clastic and carbonate strata composed of quartz sandstone,siltstone,calcareous slate and carbonate that comprise flyschoid formation. Gold mineralization is strictly controlled by a fault zone. Ore minerals are quite complex and consist of sulfides,sulfosalt,oxides,sulfate,carbonate,tungstate,telluride,native metals,and polymetallic intermetallic compounds. The diversity of mineral species in the ores and the existence of visible native gold minerals constitute outstanding features of the ore deposit.In the light of the REE distribution patterns,it is reasonably considered that the ore-forming materials of the ore deposit had affinity mainly with host rocks. S,C,Pb,H and O isotopic compositions show that the ore-forming materials were derived mainly from country rocks and underlying rocks and partly from deeper sources. Data obtained suggest that the ore-forming fluids were derived predominantly from an active meteoric groundwater system. The amount of the hydrothermal fluids in the ore-formaing and alteration system was relatively insignificant. Ore-forming temperatures are estimated to have been in the range of 120~240℃. The dissolution of ferruginous limestone in the host rocks and the sulfidation of the dissolved iron by H2S introduced by ore fluids constituted not only the most important depositional mechanism for the existence of visible gold grains but also the advantageous conditions for gold enrichment in the Zhaishang gold deposit.
【Fund】: 国家重点基础研究发展规划(2006CB403500、2009CB421003);; 国家自然科学基金(40773036);; 高等学校学科创新引智计划(B07011);; 教育部长江学者和创新团队发展计划;; 中国人民武装警察部队黄金指挥部勘查资助项目的部分成果
【CateGory Index】: P618.51
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8 CHU Kelei;MAO Jingwen;CHEN Maohong;ZHAO Jun;YU Changfa;LIN Liangzhuang;LIN Xiuguang;Institute of Mineral Resources,Chinese Academy of Geological Sciences;College of Earth Science and Resources,Chang'an University;School of Earth Sciences and Resources,China University of Geosciences (Beijing);No.719 Geological Team,Guangdong Bureau of Geological Exploration;;Source of metallogenic materials and ore-forming fluids,and metallogenic mechanism of the Yuanzhuding porphyry Cu-Mo deposit,western Guangdong Province,South China[J];Earth Science Frontiers;2013-05
9 ZHANG Fang-fang;WANG Jian-ping;LIU Chong-hao;CAO Rui-rong;CHENG Jian-jun;YANG Yong-rong;QI Feng;WANG Luo;State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences;Shaanxi Taibai Gold Mining Co., Ltd.;;The crystal forms and thermoelectricity of pyrite from the Shuangwang gold deposit, Shaanxi Province and their applications to metallogenic prognosis[J];Geology in China;2013-05
10 ZHANG ShuMing1~4,CAO ShouSun1,4,Zeng WenLe4,RAO ZeHuang1,XIE GuoFa4,FANG Xin2,ZHANG Ying2,WANG Lei2 and ZHANG Xin3(1 Key Laboratory of Radioactive Geology and Exploration Technology Fundamental Science for National Defense,East China Institute of Technology,Fuzhou 344000,Jiangxi,China;2 State Key Laboratory Breeding Base of Nuclear Resources and Environment,East China Institute of Technology,Nanchang 330013,Jiangxi,China;3 Digital Land Key Laboratory of Jiangxi Province,East China Institute of Technology,Fuzhou 344000,Jiangxi,China;4 No.261 Geological Party,Jiangxi Bureau of Geology for Nuclear Industry,Yingtan 335001,Jiangxi,China);Fluid inclusion characteristics of typical uranium deposits in Xiangshan orefield,Jiangxi Province[J];Mineral Deposits;2012-01
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Zheng Minghua Zhang Bin Liu Jianming Zhou Yufeng Gu Xuexiang Fu Renping;SIGNIFICANCE OF THE DISCOVERY OF SCHEELITE ORE-BODIES IN A GOLD DEPOSIT IN SICHUAN[J];;1993-01
2 DING Zhen-ju; LIU Cong-qiang (Institute of Geochemistry,Chinese Academy of Sciences Guiyang 550002)(China University of Geosciences, Wuhan 430074);Geochemical Characteristics of Hydrothermal Ferruginous Silica Rocks in Bikou Group:Implications for Ancient Geofluid Processes[J];ACTA SEDIMENTOLOGICA SINICA;1999-S1
3 HAN Qing, WEI Xu jun (School of Materials and Metallurgy, Northeastern University, Shenyang 110006,China);Electrodeposited Nickel-Sulfur Cathode for Hydrogen Evolution[J];JOURNAL OF NORTHEASTERN UNIVERSITY;2000-05
4 LIU Jiajun ; ZHENG Minghua; LIU JianmingZHOU Yufeng; GU Xuexiang; ZHANG Bin1) (Institute of Geochemistry, Chinese Academy of Sciences,Guiyang 550002)2 ) (Chengdu University of Technolology ,Chengdu 610059)3) (The Research Center of Mineral Resources Explo;GEOTECTONIC EVOLUTION AND MINERALIZATION ZONE OF GOLD DEPOSITS IN WESTERN QINLING[J];GEOTECTONICA ET METALLOGENIA;1997-04
5 ZOU Hai-yang, CHEN Song-ling, DAI Ta-gen(College of Resource, Environment and Civil Engineering,CentralSouth University of Technology, Changsha 410083, China);GEOLOGY AND ORE-FORMING FLUID TYPES OF THELINXIANG GOLD DEPOSIT, XUNYONG, SHANXI[J];GEOTECTONICA ET METALLOGENIA;2000-01
6 GONG Wen-jun, TAN Kai-xuan, LI Xiao-ming, GONG Ge-lian(Changsha Institute of Geotectonics, Academia Sinica, Changsha 410013, China);GEOCHEMICAL CHARACTERISTICS OF FLUID AND MECHA NISM FOR ORE FORMATION IN THE BAIYANGPINGCOPPER-SILVER DEPOSIT,YUNNAN[J];GEOTECTONICA ET METALLOGENIA;2000-02
7 FENG Jian-zhong 1 ,WANG Dong-bo 2 ,WANG Xue-ming 3 ,SHAO Shi-cai 1(1.Beijing Institute of Geology for Mineral Resources,Beijing10001,China;2.Institute of Geology,Chinese Academy of Geological Sciences,Beijing,100037,China;3.Development and Research Center of China Gelolgical Survey,Beijing,100037,China);Stable isotope geochemistry of three typical gold deposits in the West Qinling[J];Chinese Geology;2004-01
8 Liu Congqiang(Institute of Geochemistry, Academia Sinica);A FLUID INCLUSION STUDY OF YINDONGGOU Pb-Zn-Ag DEPOSIT IN THE NORTHWEST OF HUBEI PROVINCE[J];Geochimica;1989-02
9 Zhuang Hanping; Ran Chongying; Lu Jialan (① Institute of Geochemistry, The Chinese Academy of Sciences, Guiyang 550002)(② Geology Department, Kunming Institute of Technology)(③ Guangzhou Institute of Geochemistry, CAS);EXPERIMENTAL STUDIES ON INTERACTION OF COPPER,SALT AND ORGANIC MATTER[J];GEOCHIMICA;1995-S1
10 Yan Wen (South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 510301) Li Chaoyang (Open Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002);GEOCHEMICAL CHARACTERISTICS AND THEIR HYDROTHERMAL SEDIMENTARY GENESIS OF A NEW TYPE OF COPPER DEPOSIT[J];GEOCHIMICA;1997-01
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