@article{oai:ir.kagoshima-u.ac.jp:00004767,
 author = {大木, 公彦 and OKI, Kimihiko and 中村, 直子 and NAKAMURA, Naoko and 新里, 貴之 and SHINZATO, Takayuki and 内村, 公大 and UCHIMURA, Kimihiro},
 journal = {鹿児島大学理学部紀要, Reports of the Faculty of Science, Kagoshima University},
 month = {Dec},
 note = {Survey of the remains on the Korimoto campus of Kagoshima University was carried out in 2007 and 2008. At a few pit dwelling in the Tumulus period, white sand was recognized on the ground floor. This white sand is composed of almost entirely babble-walled type volcanic glass included in the Ito pyroclastic flow deposit. However white sand scarcely includes pumice and pumiceous type volcanic glass. Grain size distribution and lack of the pumiceous type volcanic glass suggest that white sand must be sorted by river water. The white sand is the secondary reworked sediments of the Ito pyroclastic flow deposits and it must have been used for keeping warm and moisture proof on the ground floor of the pit dwelling.},
 pages = {1--8},
 title = {鹿児島大学構内遺跡古墳時代竪穴住居跡の床面白砂層について},
 volume = {44},
 year = {2011}
}