摘要
在总结韩沟金矿地质特征的基础上,根据成矿物质来源、物理化学环境及成矿时代等方面的研究,认为本矿床成矿物质来自地幔和赋矿地层,成矿流体来源于岩浆水和热卤水组成的混合水。矿床成因类型属于中低温热液充填型金矿床。
Based on summarizing the geological characteristics of the Hangou gold deposit, it is believed that the ore matter of the deposit was origin in mantel and ore bearing strata and the ore fluid came from the mixed water composed of magma water and hot brine according to the research on ore matter source, physical chemical environment and ore forming era etc. The genetic type of the deposit is attributed to mesoepithermal fissure filling type of gold deposit.
出处
《矿产与地质》
2006年第4期430-433,共4页
Mineral Resources and Geology
关键词
金矿床
成因
地质特征
韩沟
河南省
gold deposit, genesis, geological character,Henan
