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cu-pb-zn
    Mechanism of Hydrothermal Convection and Alteration-Mineralization Zoning in Yinshan Cu-Pb-Zn Deposit,Jiangxi
    江西银山铜铅锌矿床热液对流与蚀变矿化分带机制
    From dacite-porphyries→Cu-Pb-Zn ore→Pb-Zn ore,the content of K~(+),Na~(+),Ca~(2+),Mg~(2+),Cl~(-),F~(-) in liquid phase of fluid inclusion is going to decline while SO~(2-)_4content is increasing,indicating more oxidability in fluid.
    从黄铁绢英岩化英安斑岩→铜铅锌矿石→铅锌矿石,液相成分中K+,Na+,Ca2+,Mg2+,Cl-,F-含量均有降低趋势,SO2-4则有升高趋势,显示流体的氧化程度增大;
    A DISCUSSION ON THE GENESIS AND OREFORMING MECHANISM OF THE HOGEQI Cu-Pb-Zn DEPOSIT
    内蒙霍各乞铜铅锌矿床成因及成矿机理
    RELATION OF VOLCANISM TO METALLOCENESIS OF YINSHAN Cu-Pb-Zn ORE DEPOSITS AT DEXING,JIANGXI PROVINE
    德兴银山铜铅锌矿床成矿作用与火山作用间的关系
    GEOCHEMICAL CHARACTERISTICS OF HUANREN SKARNTYPE Cu-Pb-Zn POLYMETAL DEPOSIT IN LIAONING PROVINCE, CHINA
    辽宁桓仁夕卡岩型铜铅锌多金属矿床的地球化学特征
    THE BASIC FEATURES AND ORE-FORMING PROCESS OF YONGPING-TONGSHAN STRATA-BOUND Cu-Pb-Zn DEPOSITS
    永平-铜山地区层控型铜铅锌矿床的成矿地质条件及其成矿作用
    Geological Features and Prospecting Potentiality for Cu-Pb-Zn Deposits in the Yanyuan Basin
    盐源盆地铜铅锌矿地质特征及找矿前景分析
    Geological Characteristics Andcriteria for Prospecting of the Jianbidong Cu-Pb-Zn Deposit in Eastern Guang Dong
    粤东尖笔岽铜铅锌矿床地质特征及找矿标志
    GEOLOGICAL CHARACTERISTICS AND GENSIS OF THE SHANGZHUANGPING Cu-Pb-Zn DEPOSIT IN HENAN AND THE GENETIC DISCUSSION
    河南上庄坪铜铅锌矿床地质特征及成因探讨
    Experiment Study on Potential Controlled Flotation for Cu-Pb-Zn Multi-Metal Sulfide Ore
    某铜铅锌多金属硫化矿电位调控浮选试验研究
    Middle-late proterozoic Era and early Palaeozoic Era are the main metallogenic epochs. In this paper, the geological features, genesis and evaluation criteria for prospecting of the superlargetype Cu-Pb-Zn deposits are emphasized.
    主要成矿时代为中晚元古代和早古生代,本文着重讨论其超大型铜铅锌矿床的地质特征、成因及找矿评价标志。
    By comparing with the similar type of Cu-Pb-Zn deposits in our country,the metallogical geological features of Cu-Pb-Zn deposits in hydrother-mal genesis of our country are discussed, and the direction of further prospecting is suggested.
    并对比我国相似铜铅锌矿床类型,探讨我国热水成因铜铅锌矿床的成矿地质特征,提出进一步找矿评价方向。
    Different ore-deposites are associated with different volcanic-intrusive rocks: the gold deposits(Cu-Pb-Zn) are usually related to middle-basic volcanic-intrusive rocks;
    不同类型的火山-侵入岩有不同的矿产:金(铜铅锌)多与中-基性火山-侵入岩有关;
    Cu-Pb-Zn, Sn(W), and Fe ore-deposits are mostly associated with middle-acidic volcanic-intrusive rocks;
    铜铅锌、锡(钨); 铁多与中-酸性火山-侵入岩有关;
    The determination of element sulphur in A. R. grade Na_2SO_4 reagent and Cu-Pb-Zn ore indicates that the proposed method has the advantages of saving time as well as very good precision and accuracy.
    用于分析纯试剂Na_2SO_4和铜铅锌矿石中S的测定表明本方法不但可大大节省分析时间,而且具有很好的准确度和精密度。
    A new reagent regime is elaboated to replace imported butyl xanthate by butyl and isopropyl aerofloats and modified lignosulphonate made in Kazakhstan for treating Cu-Pb-Zn polymetallic ores. Tests results are fairly satisfactory,and the commercial test will be done.
    提出了新的药剂制度,以国产丁基和异丙基黑药和改性木素磺酸盐取代进口的丁基黄药浮选铜铅锌多金属矿石,结果颇为满意,拟进行工业试验。
    Yongping-Tongshan stratabound Cu-Pb-Zn deposits can be dividedinto three ore zones, namely,Yujialong,Yongping and Xixiangtingzone(YongpingⅢ ore zone)according to the difference of their forma-tion mode.
    永平-铜山地区层控型铜铅锌矿床按其形成方式的差异又可分为余家垅、永平和西厢亭(永平Ⅲ矿带)三类。
    The REE patte rns are the magmatic hydrothermal characteristics in Sumugou Cu-Pb-Zn deposit.
    苏木沟铜铅锌矿点具有岩浆热液稀土元素特征。
    Based on the lead model age and the phenomenon that Cu-Pb-Zn orbodies are controlled by carbonate of the Ordovician Liuhuangshan Group,It was previously considered that the Liuhuangshan Copper-polymetallic deposit was of stratabound type formed in Ordovician.
    前人根据矿体的产出受碳酸盐岩层位控制和Pb同位素模式年龄资料 ,多认为硫磺山铜多金属矿床为层控型铜铅锌多金属矿床 ,其形成时代为奥陶纪。
    In view of the facts that the quartz porphyry in the orefield has been mineralized and the orebodies show transitional relationship with the porphyry, the authors believe that the deposit should be a porphyry Cu-Pb-Zn polymetallic one.
    基于矿区石英斑岩体见矿化和矿化蚀变 ,矿体与围岩呈渐变关系等特点 ,笔者主张该矿床属斑岩型铜铅锌多金属矿床。
 

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