广东乐昌杨柳塘铅锌矿床成矿作用分析

来源期刊：中南大学学报(自然科学版)1986年第6期

论文作者：王增润 陈子龙

文章页码：6 - 13

关键词：海相沉积； 地下热卤水； 矿源层； 层控型矿床

Key words：Submarine sedimentation； Underground hot saline brine； Source-bed； Strata-bound ore deposit

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。

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 ofevidence 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.