福建漳平北坑场钼多金属矿地质特征及成矿模式探讨  

On the Metallogenic Pattern and the Geologic Characteristics of the Beikengchang Molybdenum Polymetallic Deposit in Zhangping City,Fujian Province

作　　者：卢克标 

机构地区：[1]福建省地质调查研究院,福州350013

出　　处：《福建地质》2011年第1期6-11,共6页Geology of Fujian

摘　　要：北坑场钼多金属矿钼矿体主要分布在北坑场中粒花岗岩岩体的东南侧外接触带中,深部隐伏钼矿体连续性好,厚度大。据其地质背景、地球化学、地球物理特征及深部钻孔资料分析,探讨其成矿模式。The Beikengchang molybdenum polymetallic deposit is distributed over the southeast ouside zone of the Beikengchang medium-granitic mass.The deep concealed ore body is better in continuity and is large in thickness.Based on the analysis of the geologic background,the geochemical and geophysical character and the deep drilliog data,the author research into the metallogenic pattern.

关 键 词：钼多金属 地质特征 成矿模式 漳平北坑场 

分 类 号：P618.65[天文地球—矿床学]