凤凰山矿田成矿特征与成矿模式  

Metallogenic characteristics and metallogenic model of Lantau Peak ore field

作　　者：甘鹏 单士锋 赵晓岚 GAN Peng;SHAN Shi-feng;ZHAO Xiao-lan(Anhui geology and Mineral Exploration Bureau 321 geological team,Tongling 244051,China)

机构地区：[1]安徽省地质矿产勘查局321地质队,安徽铜陵244051

出　　处：《世界有色金属》2018年第10期250-250,252,共2页World Nonferrous Metals

摘　　要：凤凰山矿田位于长江中下游铁铜金银多金属成矿带之铜陵矿集区中部,东西向铜陵–沙滩脚构造–岩浆带与凤凰山复式向斜的复合部位,属于铜陵矿集区五大矿田之一,矽卡岩型铜金矿床产地。本文依托近年来我队在凤凰山矿田开展的一系列地质项目,总结矿田内矿床成矿特征及矿化富集因素,进而建立凤凰山矿田成矿模式,以指导今后在凤凰山矿田内找矿工作。The Lantau Peak ore field is located in the middle of the Tongling ore gathering area of the iron,copper,gold and silver metallogenic belt in the middle and lower reaches of the Yangtze River,and the compound part of the East and west to the Tongling-Beach foot tectonic-magma belt and the compound syncline of Lantau Peak,belongs to one of the five major ore fields in the Tongling ore gathering area and the origin of the skarn copper gold deposit.Based on a series of geological projects in Lantau Peak mine field in recent years,this paper summarizes the metallogenic characteristics and mineralization enrichment factors of ore deposits in the ore field,and then establishes the metallogenic model of Lantau Peak ore field so as to guide the future prospecting work in the Lantau Peak orefield.

关 键 词：凤凰山矿田 成矿特征 富集因素 成矿模式 

分 类 号：P618.2[天文地球—矿床学]