地质与资源2011，Vol.20Issue(5)：358-361,4.
辽宁四合顺硫铁矿地质特征、矿床成因与找矿标志分析
THE SIHESHUN PYRITE DEPOSIT IN LIAONING PROVINCE:Geology, genesis and prospecting indictors
赫崇刚 1孙立军2
作者信息
- 1. 辽宁省有色地质局,辽宁沈阳110003
- 2. 辽宁省有色地质局106队,辽宁铁岭112000
- 折叠
摘要
Abstract
Based on the analysis of the geological background, distribution of orebodies, characteristics of ore and altered minerals, it is concluded that the Siheshun pyrite deposit belongs to meso-hydrothermal filling and metasomatic type. The main ore-controlling and ore-forming structures are the east-west-trending faults, which are also the direction for regional prospecting. The altered mineral assemblage of silicification, sericitization and chloritization is the major indictor for ore-searching. With geophysical and geochemical anomalous features, the exploring direction is point out to achieve the prospecting breakthrough in the deep and peripheral areas.关键词
硫铁矿/中-高温热液矿床/找矿标志/四合顺/辽宁省Key words
pyrite deposit/ meso-hydrothermal type/ prospecting indictor/ Siheshun/ Liaoning Province分类
天文与地球科学引用本文复制引用
赫崇刚,孙立军..辽宁四合顺硫铁矿地质特征、矿床成因与找矿标志分析[J].地质与资源,2011,20(5):358-361,4.
