周乐尧;吴光明;刘荣;钱俊锋;徐菲琪;

• 1:浙江省地质矿产研究所
• 2:浙江省第一地质大队

摘要(Abstract)：

银山银多金属矿床主要赋存于震旦系蓝田组中。地层岩石和地球化学研究表明,矿区蓝田组沉积期间存在3个热水沉积阶段,银多金属矿床是由于热水沉积作用经后期构造叠加改造而成。区域断裂带及其两侧具有热水沉积作用特征岩石组合(含锰白云岩+硅质泥岩、粉砂岩+含硅白云质灰岩)的蓝田组是寻找本类矿床的最佳区段。

关键词(KeyWords)： 银山银多金属矿床;蓝田组;热水沉积

Abstract:

Keywords:

基金项目(Foundation): 浙江省重大科技专项重点社会发展项目“浙江省成矿构造环境与金属矿床找矿新方法”(2010C03004)

作者(Author): 周乐尧;吴光明;刘荣;钱俊锋;徐菲琪;

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DOI:

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