摘要
本文通过对拉尔玛金矿床的硫、氢、氧、铅等稳定同位素组成特征的研究，结合矿床地质特征和有关资料，对矿床成因进行了探讨，认为拉尔玛金矿属大气降水热液矿床。
Through study on constituent characteristic of sulfur,hydrogen,oxygen,lead etc inLarma gold deposit and combining with geological characteristics of this ore deposit and related data,the genesis of the deposit is discussed,believing that this deposit is a hydrdothermal one of meteoric water.
出处
《黄金》
CAS
北大核心
1995年第7期5-9,共5页
Gold
关键词
金矿床
稳定同位素
矿床成因
Larma,gold deposit,stable isotopes,meteoric water
