摘要
在总结石板沟金矿床矿化地质特征的基础上,通过对矿石氢氧同位素测试和矿石微量元素相关分析,认为成矿热液主要来源于变质水,矿床成矿环境应属低温环境,矿床成因类型属受构造剪切带控制的低温变质热液蚀变型金矿床。
The geological and metallogenic characteristics of the Shibangou gold deposit are systematically detailed in the paper. Based on the studies of mineralogy and H, O isotopes and Correlation matrix of the trace elements in ores, the metallogenic model is established. The deposit is genetically a lower temperature metamorphic hydrothermal gold deposit.
出处
《华南地质与矿产》
CAS
2008年第2期20-25,共6页
Geology and Mineral Resources of South China
关键词
相关分析
金矿床
河南石板沟
gold deposit
mineralogy
Shibangou of Henan
