摘要
大兑冲铅锌矿床隶属于大免冲－哑吧山硫化物型多金属矿带北部的一个矿床．在矿带研究基础上，重点剖析了储矿层与金属源，矿体形态、规模与控矿构造，含矿溶液与矿床的原生分带序列等的特征．进一步探讨在成矿作用过程含矿地层的地质背景和条件，金属元素分配一再分配的演化和富集规律．其目的是指导区域性的找矿和其它矿床的研究．
Dadui Chong Pb-Zn deposit belongs to the north deposit of sulfied metals ore belt from Dadui Chong to Yaba Hill.Based on ore belt study.emphasis is laid on the analysis of these characteristics such as the Pb-Zn deposit,stoney ore stratas and metallic source, the shape and dimension of orebodies and control ore structures,ore bearing solution and originalzonality sequence of deposits etc.Further discussion is about the geological background and condition of ore bearing layer and the laws of evolution and accumulation of distribution and redistribution of metallic elements in ore forming process.The aim of the study is to guide areal prospecting and study of other deposits.
出处
《昆明理工大学学报（理工版）》
1996年第3期18-24,共7页
Journal of Kunming University of Science and Technology(Natural Science Edition)
基金
国家自然科学基金
关键词
矿床特征
铅锌矿床
矿床成因
控矿构造
deposit characteristics
geological background and condition forming metallic source
metallic elements
distribute and redistribte
badui Chong sedimentary-reformation Pb-Zn deposit
