福建政和石门金多金属矿地质特征及其控矿因素  

Discussion on Geological Characteristics and Control Factors of the Shimen Au-polymetallic Deposit in Zhenghe County,Fujian Province

作　　者：龚萍[1] 

机构地区：[1]福建省闽北地质大队,邵武354000

出　　处：《福建地质》2006年第1期18-24,共7页Geology of Fujian

摘　　要：政和石门金多金属矿成矿地质条件有利,找矿前景好。以区域成矿地质背景、矿产地质特征为基础,从地层、构造、岩浆作用,特别是中生代火山活动等方面,系统地分析了该区金多金属矿产的控矿因素。Mineralization geological condition of the Shimen Area in Zhenghe County is favorable for Au-polymetaltic deposit, which has prospect well to find Au-polymetallie ore deposits, Based on the regional metallogenetic geology background and minerals geologic Characteristics, especially volcanic activity in Mesozoic in this area, the control factors for Au-polymetallic deposit were systematically analyzed.

关 键 词：金多金属矿 地质特征 控矿因素 政和石门 

分 类 号：P618.2[天文地球—矿床学]