摘要
This paper indicates that Au ore intensive district in northwestern Jiaodong is related to deep ore-controlling structures. After experiencing evolution of long stable platform during Paleozoic, the eastern area of North China Platform entered the stage of mantle plume evolution in Yanshanian movement period. This produced an external ore intensive zone containing Jiudian-Xiadian-Dayinggezhuang-Qixia-Rushan deposits surrounding the Laiyang-Laixi mantle plume, and an internal ore intensive zone consisting of Jigezhuang-Sanshandao-Jiaojia-Linglong-Daliuhang-Xiejiazhuang-Quhezhuang deposits. Both ore intensive zones constitute a series of orefield-ore deposits-ore veins assemblages.