摘要
概述了区域地质特征和控矿地质条件，并较详细地叙述了矿床地质特征。提出了本矿床成因的新观点为中一低温构造热水溶液充填一渗滤、扩散矿床。
The regional geology and ore -control conditions are introducedbriefly at first, and then the geological characteritics are described in detail. The new view about the ore genesis is put forward as follows: The deposit belong among the filling - percolation and diffusion of tectonic hydrothermal solution in middle - low temperature
关键词
重晶石矿床
地质特征
成因
Geological characteristics Ore genesis Tectonic hydrothermal solution Shigou
