为扩大金厂矿区找矿范围，应加强对金厂矿区外围找矿力度和综合研究程度。根据前人对金厂矿区地质特征的调查研究，金厂矿区矿化体受花岗岩体、闪长岩体和NE、NW、近SN向断裂控制。通过对大徐山矿权区成矿元素进行描述性统计、R型聚类分析和因子分析得出，矿权区前缘晕及尾晕指示元素呈强富集程度，存在多期次多阶段成矿作用。类比金厂矿区矿体特征、成矿模式、成矿规律和找矿标志，认为金厂矿区外围大徐山矿权找矿方向为矿权区东、西部天桥岭组及托盘沟组与燕山期花岗斑岩岩组、花岗闪长岩、闪长玢岩岩组的接触部位，显示大徐山矿权区具有较大的找矿潜力。

In order to expand prospecting range at the Jinchang deposits，it is necessary to strength the comprehensive investigation and prospecting efforts in the deposits surrounding areas.According to previous research，it was believed that mineralized bodies in the Jinchang deposits was controlled by the granodiorite and diorite and the North-east，also the North-west and the nearly South-north trending fault.Through comparing the metallogenic element descriptive statistics，R-cluster analysis and factor analysis，it is found that the front halo and tail halo indicator elements in the mineral rights area belong to strong enrichment degree，and there are several stages of mineralization.By analogy the ore deposit，metallogenic model，metallogenic regularity，prospecting marks of Jinchang deposits，it is suggested the eastern and western region of the mine，and the contact region between Tianqiaoling Group，Tuopangou Group and Yanshanian granite porphyry intermediated-acidic Group，corcovadite，granodiorite porphyrite have greater prospecting potential.