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邓家山铅锌矿床物质成分及矿床成因的探讨
引用本文:许凤仪.邓家山铅锌矿床物质成分及矿床成因的探讨[J].兰州大学学报(自然科学版),1989,25(3):133-142.
作者姓名:许凤仪
作者单位:甘肃省有色金属地质二队
摘    要:

关 键 词:铅锌矿床  物质成分  矿床成因

The Opproach to the Material Component and Metallogeny of Denjiashan lead and Zine Deposits
Xu Fengyi.The Opproach to the Material Component and Metallogeny of Denjiashan lead and Zine Deposits[J].Journal of Lanzhou University(Natural Science),1989,25(3):133-142.
Authors:Xu Fengyi
Abstract:Denjiashan lead and zinc deposits occured between biogenic limestone andphyllite.The mineral source formation was deposited in limited shallowbasin behind the reef under the tide during syndeposition.The industrialore bodies were formed during reformation.Sphalerite and galena are do-minant minerals.Five silverbarring minerals were identified.Besides pband Zn,useful eomponents such and Ag,Cd,Ge,as Ga may be madecomprehensive use of.The essay deseripts the material components and the occuring stateof associated elements of the ore deposits,presents briefly the view onmetallogeny,the research on the ore controls,including stratum,litholo-gical characters,biostrata,lithoracies and structure,and shows that thedeposit belongs to a strata-bound ore deposit of sedimentary and reformative type.
Keywords:Denjiashan  Lead and Zinc deposits  Material component  Metallogeny  
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