江西浮梁葫芦尖锡矿地质特征及外围找矿前景分析  

Geological characteristics of Hulujian tin deposit and its exploration perspective in its periphery area,Fuliang county,Jiangxi Province

作　　者：刘九金[1] 黄韶春[1] 梅惠呈[1] 

机构地区：[1]江西省地矿局九一五地质大队,南昌330002

出　　处：《资源调查与环境》2013年第1期44-52,共9页Resources Survey & Environment

摘　　要：本文介绍了葫芦尖锡矿区区域地质背景、锡矿体的地质特征,系统阐述了地层、构造和岩浆岩地质特征。通过重点分析该矿区及外围地区的找矿前景,发现葫芦尖矿区构造蚀变岩带是重要的找矿标志,认为莲花山(潘村)——鄣公山地区成矿地质条件优越,锡多金属矿找矿潜力巨大,进一步在该地区进行锡多金属矿找矿、勘查工作都将对找矿突破产生积极的促进和指导作用。This paper introduces the regional geological background and geological characteristics of tin orebodies in the Hulujian tin deposit, and systematically describes the geological features of strata, structures and magmatic rocks in the area. By analyzing the exploration perspective of this mineralized area and its periphery area, it is found that the structural altered rock belts in the Hulujian mineralized area are the most important ore-prospecting criteria. We consider that the Lianhuashan（Pancun） Zhanggongshan region shows favourable metallogenic geological condi tions and enormous potential of prospecting tin-polymetallic ores, and therefore the further prospecting and exploration work on the tin-polymetallic ores in the area will positively make promotion and guiding effects for the im portant breakthrow of prospecting in this area.

关 键 词：鄣公山 地质特征 构造蚀变岩带 找矿前景 

分 类 号：P618.44[天文地球—矿床学]