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广东乐昌杨柳塘铅锌矿床成矿作用分析
引用本文:王增润,陈子龙.广东乐昌杨柳塘铅锌矿床成矿作用分析[J].中南大学学报(自然科学版),1986(6).
作者姓名:王增润  陈子龙
作者单位:中南矿冶学院地质系,中南矿冶学院地质系
摘    要:作者通过野外及室内综合研究,对该矿床地质地球化学特征、成矿物质来源、成矿作用过程及成矿作用方式等问题进行了较全面的探讨,以较充分的证据说明该矿床属海相沉积(可能含部分远源海底火山喷发沉积)-地下热卤水改造成因的层控型矿床。文中并指出了找矿方向。

关 键 词:海相沉积  地下热卤水  矿源层  层控型矿床

AN ANALYSIS OF THE MINERALIZATION OF THE LEAD-ZINC ORE DEPOSITS IN YANGLIUTANG,LECHANG,GUANGDONG
Wang Zengran,Chen Zilong.AN ANALYSIS OF THE MINERALIZATION OF THE LEAD-ZINC ORE DEPOSITS IN YANGLIUTANG,LECHANG,GUANGDONG[J].Journal of Central South University:Science and Technology,1986(6).
Authors:Wang Zengran  Chen Zilong
Institution:Wang Zengran;Chen Zilong Department of Geology
Abstract:The origin of the lead-zinc ore deposits in Yangliutang of Guangdong is similiar to that of the Fankou lead-zinc ore deposits in Guangdong.The features of geochemistry,the resourses of the ore-forming material,the processcs and depositional types of the mineralization of the ore deposits are studied and determined.A lot of evidence indicate that the ore deposits may be referred to the strata-bound ore deposits which were formed by submarine sedimentation(probably partly volcanic sedimentation of far-off resourses)and the reformation of underground hot saline brine.The directions in researching for new ore deposits in this area are also suggested in this paper.
Keywords:Submarine sedimentation  Underground hot saline brine  Source-bed  Strata-bound ore deposit
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