Wangwangzhuang deposit is a concealed skarn-iron deposit in Shandong

which is in Jinling diorite intrusive contact of Ordovician carbonate rock belt. It is the hydrothermal metasomatic deposit and has strata-bound characteristics. Its formation by the late Yanshanian magmatic intrusion to pure limestone in the Ordovician of Wangwangzhuang seat

leaving a large number of contact metasomatic iron enrichment and mineralization. The geological characteristics of the ore was analyzed

explore its metallogenic regularity

summing up the metallogenic model

so that provides some references for the same type of iron ore resources in the further development of regional.