摘要
在论述龙山金锑矿矿床地质特征的基础上,从成矿物质来源,硫、氧同位素特征,黄铁矿标型特征及成矿温度等方面阐述了成矿地质条件。探讨了矿床成因。提出该矿矿床为沉积—变质热液矿床的认识。
The geological features of this deposit are systematically described. Mineralization conditions, sources of ore material and metallogenetic mechanism are also analysed with respect to sulfur and oxygen isotope composition, pyrite typomorphic feartures and fluid inclusion thermometry data. In conclusion, it is suggested that this deposit is a sedimentary -metamorphic hydrothermal deposit.
出处
《矿产与地质》
1990年第2期21-24,共4页
Mineral Resources and Geology
