云南省落乌铜铅磷矿地质特征与找矿标志研究  

Study on geological characteristics and prospecting criteria of Luowu copper-lead-phosphorus deposit in Yunnan Province

作　　者：包昆[1] BAO Kun(Yunnan College of Tourism Vocation,Kunming 650221,Yunan,China)

机构地区：[1]云南旅游职业学院

出　　处：《资源信息与工程》2020年第1期13-16,共4页Resource Information and Engineering

摘　　要：矿区位于白龙塘向斜北翼,断裂主要发育有北西向和北东向两组。铜、铅矿床主要赋存于构造破碎带中。盆地中磷质的聚集是多期的,依次接受磷酸盐→碳酸盐→碎屑岩沉积,寒武系渔户村组为矿区内磷矿赋存层位。The mining area is located on the north of the Bailongtang syncline, and the faults develop mainly in the north-west or north-east direction. Copper and lead deposits are mainly in the structural fracture zones. The accumulation of phosphorous in the basin is multi-phase, which is deposited by phosphate, carbonate and clasolic successively. The Cambrian Yuhucun Fm is the phosphate ore occurrence layer in the mining area.

关 键 词：找矿标志 赋存层位 地质特征 渔户村组 构造破碎带 铅矿床 北西向 北东向 

分 类 号：P618[天文地球—矿床学]