长江中下游成矿带(江苏段)硫铁矿床成矿模式  

Metallogenic models of pyrite deposits in the middle and lower Yangtze River metallogenic belt,Jiangsu Province

作　　者：黄震[1] 姜丽[1] 王海欧[1] 来又东[1] 魏芳[1] 

机构地区：[1]江苏省地质调查研究院,南京210018

出　　处：《资源调查与环境》2015年第3期165-171,共7页Resources Survey & Environment

基　　金：中国地质调查局"江苏省(含上海市)矿产资源潜力评价"项目(项目编号:1212010881615;1212011121007)资助

摘　　要：通过分析长江中下游成矿带(江苏段)区域成矿地质条件、硫铁矿典型矿床及区域成矿特征,建立了陆相火山岩型和矽卡岩型硫铁矿床成矿模式。结合典型矿床成矿、物化探异常特征,提出长江中下游成矿带(江苏段)硫铁矿床找矿模型,这对于该区域找矿预测具有指导意义。Based on the study of regional metallogenic conditions, typical pyrite deposits and regional mineralization characteristics of the middle and lower Yangtze River metallogenic belt, Jiangsu Province, we establish metallogenic models of continental volcanic-type and skarn-type pyrite deposits in this paper. Combined with the characteristics of mineralization and geophysical-geochemical anomaly of some typical deposits, we propose metallogenic models of pyrite deposits in the middle and lower Yangtze River metallogenic belt, Jiangsu Province, which has guiding significance for regional prospect prediction in this area.

关 键 词：硫铁矿床 成矿特征 成矿模式 找矿模型 长江中下游成矿带 

分 类 号：P618.31[天文地球—矿床学]