岡山大学 地球科学研究報告
Published by Okayama University Earth Science Reports Editorial Committee

岡山平野の泥炭層から推測される完新世の海水準変動と古環境変遷

鈴木 茂之 岡山大学理学部地球科学科
抄録
Quaternary peat beds from bore-hole samples deliver information to reconstruct paleoenvironment. Altitudes of dated non-marine peat beds and marine beds allow to be created a sea-level curve. 4 peat beds (A to D) are identified from the uppermost Pleistocene to Holocene deposits of the Okayama Plain. They thought to be deposited at stable events during sea-level change.
キーワード
Holocene
peat beds
paleoenvironment
sea-level change
Okayama Plain
ISSN
1340-7414
NCID
AN10506284
NAID