摘要
对桂北白桦岭金矿区黄铁矿晶体形态、热电性研究表明，｛ｈｋｏ｝及其聚形晶含量高，Ｐ导型热电均值大为富矿标志，矿液来源于ＮＥ，并向ＳＷ流动，西部剥蚀程度较强，杨柳棚、观音山、挂耙山、燕子窝深部较有远景。
According to the research on the crystal form and thermoelectricity of pyrite, it is indicated that {hko} and its combinate forms high content and big average value of thermoelectricity of P are marking of rich ore bodies. Metallogenetic hydrothermal solution comes from NE and flows towards SW. It strongly eroded at the western area. It has a good prospect to Yangli upeng, Guanyinshan, Guapashan and Yanziwuo.
出处
《桂林工学院学报》
1996年第1期26-29,共4页
Journal of Guilin University of Technology
关键词
金矿床
黄铁矿
找矿
矿物学
gold deposit, Pyrite, genetic mineralogy, prospecting mineralogy, Guangxi
