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招掖金矿带位于沂沭断裂带东侧,胶北隆起西北端栖霞复背斜北翼,受东西向阜山背斜控制.金矿床受新华夏系北东向压扭性断裂与东西向构造复合部位控制,金矿带内地层主要为上太古界-下元古界胶东群,其下部蓬夼组是金矿带的主要层位,分布于混合花岗岩体的周边地段.中部民山组零星分布于矿带北部边缘;上部富阳组分布于招掖以东.胶东群地层走向为东西-北西西
The gold belt of Zhaoye is located east of the Yishu fault zone and is controlled by the east-west Fushan anticline to the north wing of the Qixia anticlinorium at the northwestern margin of the Jiaobei uplift.The gold deposit is controlled by the NE- Tectonic assemblage control, the inner strata of the gold belt are mainly the Upper Archean-Lower Proterozoic Jiaodong Group, and the lower Penglao Formation is the main strata of the gold belt distributed in the periphery of the mixed granite body. Sporadically distributed in the north edge of the ore belt; the upper Fuyang Formation is distributed to the east of Zhaye. The Jiaodong Formation stratigraphy is east-west