层控矿床是国际矿床学界近十余年来讨论最热烈的问题之一。我国层控矿床十分发育,其中汞矿也具有典型的层控特征。这些矿床的成因研究目前正受重视,传统的成因观点也被怀疑。近几年,人们普遍认为中国多数汞矿应属“沉积-地下水热液”或“沉积改造”成因。但是,对于这种矿床成因观点的一些具体问题,例如在成矿的第一阶段中,元素的表生迁移搬运、元素的初步沉积富集或使这些元表生富集到形成矿床的机制等,直到目前,研究仍然甚少。本文的目的在于通过探讨,深化对汞矿成因的认识。 Stratum controlling deposit is one of the hottest issues discussed in the international deposit field for more than ten years. The stratiform deposit in our country is very developed, and the mercury deposit also has typical stratification control features. The genesis of these deposits is currently being taken seriously, the traditional causes of formation are also suspected. In recent years, it is generally accepted that most of the mercury mines in China should belong to the “sedimentary-hydrothermal hydrothermal” or “sedimentary transformation” causes. However, some specific questions about the origin of this deposit, such as the migration and transport of the elements in the first stage of metallogenesis, the preliminary deposition and enrichment of elements or the enrichment of these elements into the deposit formation mechanism, etc. Until now, there are still few studies. The purpose of this article is to deepen our understanding of the genesis of mercury deposits through exploration.