会东淌塘铜矿矿床成因分析及其找矿方向

Tung Tong drip copper ore genesis Analysis and Prospecting

会东淌塘铜矿矿区地层为元古界会理群淌塘组,主要岩性为炭质绢云千枚岩、绢云千枚岩、炭质千枚岩、绢云千枚岩等浅变质岩组成,该矿床为埋藏较深的小型隐伏矿,在地质勘探期间一直认为矿区总体上是一单斜地层,按照这一指导方针圈定的矿体与矿山开采所揭露的矿体出入较大,笔者结合近年来矿山收集到的实际地质资料,对矿区地质特征做了系统的总结和描述,对矿区总体构造进行了重新认识,对矿体特征进行了重新总结,对矿床成因提出了新的探讨和研究,并就矿山后续地质找矿提出找矿建议。

Will the East drip Tong copper mine strata of Proterozoic group mobility Tong ttuili Group,the major iithology of carbonaceous phyllite cloud silk,silk cloud phyllite,carbonaceous phyllite,silk cloud phyllite and other low-grade metamorphic composition,the deposit is a small hidden mines buried deep in the geological exploration has been considered during the whole mining area is a monocline strata,in accordance with the guidelines of the ore body delineation and mining of the ore body exposed by access to large,the author collected from the mines in recent years,with the actual geological information on the mine#39;s geological features of the system to do a summary and description of the overall structure of the mine was re-understanding of the ore body characteristics of the re-summed up on the genesis of the proposed The new exploration and research,and follow-up on the mine geological prospecting prospecting make recommendations.