Abstract:Porcelain stone in Fengjiacun village occurs in thin spots in the late Mesozoic Yanshan monzonite porphyry, and belongs to acidic intrusive rocks shallow deposits. Its chemical composition is high silica, alkalirich, and poor iron and magnesium. This deposit belongs to magmatic deposit type. Ore bodies outcropped in the surface with the advantages of large scale, superior quality and easy exploitation. This deposit not only provide resources support for the development of ceramic industry in Shandong province, but also has important practical significance for exploring the same type porcelain stone deposit.