摘要
四川省理塘县宗巴金多金属矿位于甘孜-理塘构造带中南段。区内主要出露曲嘎寺组地层;金矿化体赋存于曲嘎寺组的次级构造蚀变带中,围岩为板岩或千枚岩,含金构造蚀变带由构造蚀变岩和充填于断裂构造破碎带中的石英脉组成,总体呈透镜状沿北西南东向展布,脉群沿走向延伸长约180m,平均品位3.8g/t,具有进一步开展勘查工作的潜在价值。
Zong Ba Gold polymetallic deposit is located in the south section of Ganzi Litang tectonic belt, Litang County, Sichuan Province. Within the mining area exposed Qu GA Temple strata; The gold ore bodies occur in Qu GA Temple group of secondary structure alteration zone in, surrounding rock for slate and phyllite, gold bearing tectonic erosion variable by tectonic erosion change rock and filling in fault broken zone of quartz veins with, the overall trend of lenticular along the southwest of the North East trending and vein group along strike with an extension of about 180 m, the average grade of 3.8g/t with further development of the potential value of the survey work.
出处
《世界有色金属》
2016年第6期156-157,共2页
World Nonferrous Metals
