摘要
百花岭矿区与金堆城超大斑岩型钼矿床同属于一个构造单元,其北部的浅成低温热液矿床为金堆城斑岩型钼矿床顶部或外围,具有形成大型金多金属矿的条件。
The Baihualing mineralized area and the Jinduicheng super large-sized pophery molybde- num deposit are situated in a same tectonic unit, of which the northern shallow low-temperature hy- drothermal deposits are distributed at the top and/or the periphery of the Jinduieheng molybdenum deposit. In this region, large scale-sized deposits are possible under the metallogenic conditions.
出处
《陕西地质》
2015年第2期56-62,共7页
Geology of Shaanxi
关键词
地质特征
控矿条件
找矿前景
成矿模式
geology
ore-controlling
ore prospective
metallogenic model
