CAJ | 학술논문

通过对铁炉坪银铅矿床地层、构造、岩浆岩及围岩蚀变等地质特征研究，认为矿体受花岗绿岩带及构造断裂带的联合控制，并受后期热液叠加改造，属海底火山喷发-变质热液改造块状硫化物型矿床，归纳总结其找矿标志，对熊耳山地区寻找同类型矿床具重要指导意义。
통과대철로평은연광상지층、구조、암장암급위암식변등지질특정연구，인위광체수화강록암대급구조단렬대적연합공제，병수후기열액첩가개조，속해저화산분발-변질열액개조괴상류화물형광상，귀납총결기조광표지，대웅이산지구심조동류형광상구중요지도의의。
Based on the research of the geological features of Tieluping silver-lead deposit such as deposit stra-tum,formation and the alteration of the magmatite and country rock,it is believed that the ore body is con-trolled by both of granite greenstone belt and tectonic fault zone and reconstructed by late hydrothermal su-perimposition.It can be categorized as massive sulfide deposit of submarine volcanic eruption-metamorphic hydrothermal reconstruction.The prospecting indicators which summary will have an important guiding sig-nificance for exploring the same type of deposit at Xiong'er area.