摘要
作者通过对老王寨金矿床成矿地质背景、金矿化特征、成矿物质来源、成矿流体性质、成矿过程的详细研究，认为矿床是在该区深部地质过程中深源热流体作用的产物，由此提出深源流体成矿的新见解。
The writer studied the geological setting,characters of gold deposit,Au-source,mineralizer-source, fluid-source and its properties and ore- forming process.It showsthat genesis of the gold deposit was resulted from a deep fluid that was in mineralizer such asCl-.CO2 and S2-.So this paper first advances a new view that is deep fluid metallogent.
出处
《物探化探计算技术》
CAS
CSCD
1996年第S1期17-20,共4页
Computing Techniques For Geophysical and Geochemical Exploration
基金
国家科委攀登计划"超大"项目
中国科学院矿床地球化学开放研究实验室基金
关键词
金矿床
成因
深源流体
成矿
gold deposit, genesis, deep filud,metallogeny.
