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文峪金矿床是小秦岭金矿带内一大型裂控石英脉型矿床，５３０脉是其主要矿脉之一，其走向近东西，倾向南，倾角中等。受断裂产状空间变化及成矿期控矿断裂运动方式的影响，其内含金石英脉体多产于控矿断裂带２５０～２７０°走向段及４０～５０°倾角段。Ⅱ、Ⅲ主成矿阶段主要迭加发育于控矿断裂带内２６０～２７０°走向段及４５～５０°倾角段等有利构造空间部位。这一规律对指导该区相同产状矿脉的找矿勘查评价工作具重要意义。
Wenyu gold deposit is a large schistogenic quartz vein type deposit in the Xiaoqinling gold belt. The 530 veins are one of the main veins. The Wenyugu gold deposit is close to the east and west, with a tendency of south and moderate dip. Affected by the spatial change of fracture shape and the ore-controlling fault movement during mineralization, the gold-bearing quartz veins are prolific in the 250-270 ° strike and 40-50 ° sections of the ore-controlling fault. The main ore-forming stages Ⅱ and Ⅲ are mainly superimposed on favorable structural space such as 260 ° -270 ° strike and 45 ° -50 ° dip in the ore-control fracture zone. This law is of great significance to the prospecting and evaluation of the same type of ore veins in the area.