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黄沙坪铅锌多金属矿床的成因分析
引用本文:谷俐.黄沙坪铅锌多金属矿床的成因分析[J].湖南地质,1997,16(4):232-235,238.
作者姓名:谷俐
作者单位:中国科学院长沙大地构造研究所
摘    要:黄沙坪铅锌多金属矿床的单矿物包裹体:测温,气液成分和微量元素分析结果,结合矿床硫,铅同位素组成及同位素地质年龄的综合分析表明,该矿床的成因以岩浆热液成矿为主,兼有沉积层控矿床特征。

关 键 词:铅矿床  锌矿床  多金属矿床  成因分析

On the Genesis of the Lead Zinc Polymetallic Deposit in Huangshaping
Gu LiChangsha Institute of Geotectonics,Academia Sinica.On the Genesis of the Lead Zinc Polymetallic Deposit in Huangshaping[J].Hunan Geology,1997,16(4):232-235,238.
Authors:Gu LiChangsha Institute of Geotectonics  Academia Sinica
Abstract:By means of many analysis including thermometry and gasliquid composition in inclusions,and trace elements in single minerals,and on the basis of types of deposits in the district,S and Pb isotope compositions and isotope chronology,this paper has studied the genesis of the Pb Zn polymetallic deposit in Huangshaping and drawn a conclusion that the deposit has mainly a magmatic hydrothermal origin with the feature of sedimentary strata bounded mineralization.
Keywords:Lead  Zinc deposit  genesis of deposit  magmatic hydrothermal solution  strata  bounded deposit  Huangshaping  
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