在无产阶级文化大革命的推动下,经过近年来的工作,现已查明本矿床是一个伴生有铜、钴和铂族元素的规模较大的镍矿床,使以往被否定了的矿区获得了新生.本文着重介绍矿床的地质特征,并对其成因提出初步看法.一、矿区地质概况该矿床位于康滇台背斜北部.区内主要构造为一轴向近南北的背斜.含镍岩体均产 Driven by the Great Proletarian Cultural Revolution and after years of work, it has been ascertained that the deposit is a large-scale nickel deposit associated with copper, cobalt and platinum group elements that have given birth to newborn mines that were previously denied This article focuses on the geologic characteristics of the deposit and gives a preliminary view on its cause I. Geological Profile of the Mining Area The deposit is located in the northern part of the Kangndiantai anticline, and the main structure in the area is an anticline nearly north-south anticline. Are produced