Abstract:The division by rock-statum of Quaternary in Shandong province has made advances in recent years, which can be stated as follows: thick loess deposits formed in middle to late Pleistocene period have been differentiately divided into Yanglanhe formation and Dazhan formation; Paleolake-marsh sedimentary in early Holocene into Heituhu formation. New recognization and information have been gained in many aspects: such as diachronous phenomenon, chronostratic classification and geological development history, e...