辽宁兴城碱厂一带金、多金属成矿地质特征及找矿前景

Metallogenetic geological features and prospective analysis of Jianchang of Xingchong,Liaoning Province

通过对兴城碱厂地质概况的认识,结合区域物理、化学异常特征,为本区寻找铜钼矿床奠定了基础。区域性断裂构造影响了成矿带中的岩浆分布,沿断裂发育的蚀变带及硅化细脉带,是本区的控矿和赋矿构造,其中北东向断裂多被岩脉及铜钼矿化硅化脉充填,是本区找矿的有利部位。

On the basis of the metallogenetic geological features a regioncal physicochemical anomalous characteristic,determined prospecting direction for copper-molybdenum deposit in the study area.The regional faulted structure affected magmatic distribution in the metallogenic belt.The alternation zone and solicited veined zone along the faulted zones,among them,the most of NE faults are filled by the veins and Cu-Mo mineralized silicified veins which is a favorable prospecting location in the study area.