CAJ | 학술논문

云南省弥勒县铜矿处于弥勒-师宗深断裂南部NE构造带上,矿区主要含矿地层为二叠系上统峨眉山玄武岩组和下统栖霞茅口组. 二叠世晚期后,该地区长期处于陆地,侵蚀作用明显,喀斯特地貌发育. 通过分析认为该区主要为土壤型风化沉积改造矿床,以喀斯特地貌为基底有玄武岩风化堆积物的地区和灰岩有利部位为有利找矿地段.
운남성미륵현동광처우미륵-사종심단렬남부NE구조대상,광구주요함광지층위이첩계상통아미산현무암조화하통서하모구조. 이첩세만기후,해지구장기처우륙지,침식작용명현,객사특지모발육. 통과분석인위해구주요위토양형풍화침적개조광상,이객사특지모위기저유현무암풍화퇴적물적지구화회암유리부위위유리조광지단.
The copper mine of Mile country located in the deep fracture that on the south of Maitreya-Shizong structural belt,the area of mining formation is primarily contain permian series emeishan ba-salt formation and Qixia under the Maokou. After the late permian,the area of land in the long-term, significant erosion,karst landforms. By analyzing the type of soil that the area is mainly weathered sedimentary deposit transformation in karst region of the substrate has weathered basalt and limestone deposits favorable position for enabling prospecting area.