云南省金平县中良铜镍多金属矿床地质特征及找矿标志

金平县中良铜镍多金属矿床位于云南哀牢山结晶基底断块东南端，为岩浆结晶分异和岩浆熔离矿床。为查明矿体特征，扩大找矿成果，通过地质、物探、化探及地表工程揭露等技术手段对矿体进行了查证，在沿NW向F1断层侵位的基性-超基性杂岩体中圈定出铜镍矿体和铁矿（化）体。通过在分析矿床地质特征基础上，笔者认为研究区内的基性-超基性杂岩体，NW向分布的断裂带，Cu、Ni、Co、V、Ti等元素的土壤地球化学异常区，地表出露的皮壳状、蜂窝状铁帽是矿床重要的找矿标志。

Geological Characteristics and Prospecting Criteria of Zhongliang Copper Nickel Polymetallic Deposit in Jinpin County in Yunnan Province

Zhongliang copper nickel polymetallic deposit in Jinping county is located in the southeast of crystalline basement fault block of Ailaoshan Mountain in Yunnan province. It is a magmatic crystallization differentiation and liquation type. In order to identify characteristics of the ore bodies and expand prospecting outcomes, bt using geological, geophysical, geochemical and surface engineering methods, the ore bodies have been identified. Copper nickel ore bodies and iron ore (mineralized) bodies have been delineated in the mafic ultramafic complex intruded along the NW trending F1 fault. Based on the analysis of geological characteristics of the deposit, it is believed that the basic ultrabasic complex in the study area, the NW trending fracture zone, the soil geochemical anomaly area of Cu, Ni, Co, V, Ti and other elements, and the crust and honeycomb shaped gossans exposed on the surface are important prospecting indicators in the study area.