Abstract:Jiaodong Mesozoic gold deposit within the formation of many types, are widely distributed. Article from the perspective of oreforming system components to the type of gold deposit, occurrence, distribution characteristics, such as forming the basis of depth, combined with the Mesozoic regional tectonic setting, structural evolution, focusing on the Shandong gold mineralization sources, mineralization, mineralization period transformation. Shandong Gold Mining pool is the root cause of the formation of Mesozoic tectonic regime on the transition region, the Mesozoic tectonic regime transformation is one of the manifestations. Various types of gold deposits in the context of a unified structure, oreforming fluids rise along the channel structure formed by a variety of hydrothermal deposits, deposit distribution from lithology, and tectonic activity and is closely related to the same period. Earth differentiation in the early formation of the early Mesozoic lower crust has a high degree of value Jinfeng ancient Archean and Proterozoic continental nucleus is Jiaodong ancient continental crust material basis of gold mineralization (ore source rocks). Oreforming process because of the crust, mantle interaction leads to forming fluid component complex, diverse sources. Jiaodong future gold exploration, and has broad prospects, future exploration should be guided by the theory, efforts to expand the exploration of patterns and types of mineral deposits.
