浅成低温热液贵金属矿床成矿条件浅析

Metallogenic conditions of epithermal noble metal deposits

浅成低温热液贵金属矿床是由于火山活动产出的贵金属物质在低温热液的环境下,火山浅层岩体系统浅部形成的矿床。随着近些年发现的众多浅成低温热液贵金属矿床,使得这种矿床成为了世界各国科学家的研究热点。在科学家对浅成低温热液贵金属矿床成矿条件不懈研究下,这种贵金属成矿的岩浆条件以及成矿机理等方面已经较为清晰的展现在人们的面前,这为以后贵金属矿床的发现和研究提供了可靠依据。

The epithermal precious metal deposit is a deposit formed in the shallow part of the volcanic shallow rock mass system under the environment of the low-temperature hydrothermal. With the discovery of many epithermal precious metal deposits in recent years, this deposit has become a research hotspot of scientists all over the world. Under the unremitting study of the metallogenic conditions of epithermal precious metal deposits by scientists, the magmatic conditions and metallogenic mechanism of this kind of precious metal deposits have been clearly displayed in front of people, which provides a reliable basis for the future discovery and study of precious metal deposits.