摘要
西洋坂金矿16个矿(化)体均产于其矿源层葛坑组变质岩中,属变质热液型,根据地层、构造、土壤地球化学异常分析,区内北东、北西向断裂交汇处及其深部有找到新的金矿前景。
The 16 orebodies or mineralizing bodies in the Xiyangban gold mine exist in the middle and late Proterozoic metamorphic rock which is the source bed of the gold mine. The Xiyangban gold mine belongs to the type of metamorphic-hydrothermal solution. Based on the analyses results of the strata, structure and pedogeochemical anomaly, it is possible to hunt for a new gold mine in the northeastern and northwestern fault interjunction and the deep part of the surveyed area.
出处
《福建地质》
2010年第2期107-110,共4页
Geology of Fujian
关键词
金矿
地质特征
找矿前景
德化西洋坂
gold mine, geologic characteristics, ore-finding perspective, Dehua County