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.
出处
《福建地质》
2011年第1期6-11,共6页
Geology of Fujian
关键词
钼多金属
地质特征
成矿模式
漳平北坑场
molybdenum polymetallic
geologic characteristics
metallogenic pattern
the Beikengchang in Zhangping city