The Chuseki formation, latest Pleistocene to Holocene sediments, of the lowland in the basin of Shiribeshi-toshibetsu River, Oshima Peninsula, Hokkaido - Relation between the remains on the lower terrace and ultra-soft mud bed in hypsithermal interval of postglacial age -

Authors=OKA Takao

Journal/Book_names=Report of the Geological Survey of Hokkaido

number=80

pages=63-109

Publish_year=2009

Publish_Country=JPN

Publisher=Geological Survey of Hokkaido

Language_of_Text=JA

Language_of_Abs=EN

ISSN=13453815

ID=200924042