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兴隆钨钼矿床属高中温热液矿床,矿体呈脉状产于燕山期花岗岩的断裂之中,矿体与云英岩化和硅化关系密切,矿化类型主要为石英脉-蚀变岩型,矿体主要受北西向构造控制。本文总结了矿床地质特征和成矿规律,确定了该区矿床的找矿标志。
The Xinglong tungsten-molybdenum deposit belongs to the high-temperature medium-temperature hydrothermal ore deposit. The orebody is vein-shaped in the fault of Yanshanian granite. The orebody is closely related to the phlogoyalization and silicification. The mineralization types are mainly quartz vein-altered rock type The ore body is mainly controlled by the NW structure. This article summarizes the geological characteristics and metallogenic regularity of the deposit and determines the prospecting sign of the deposit in the area.