倉敷市水島地域の沖積地盤地質
スポンサーリンク
概要
- 論文の詳細を見る
The study srea, Mizushima is occupied by polder and reclaimed land. The ground of this area is composed of the Holocene deposits below the surface. The deposits are mostly 10 to 20m in thickness and composed of 2 units, the B Unit and C&D Unit. The B Unit is composed of muddy sand with 2 to 3m in thickness. This unit is thought to be deposited in the mouth of paleoriver. The C&D Unit is composed of marine mud and sand with 10 to 15m in thickness. This unit is especially soft and will expand ground oscillations during an earthquake.
- 岡山大学理学部地球科学教室の論文
- 2006-03-31
岡山大学理学部地球科学教室 | 論文
- 太平洋東部赤道海域における二酸化炭素分圧の増加速度
- 西表島船浦湾におけるマングローブ干潟の堆積環境 ―堆積物と生物遺骸の保存状況について―
- 岡山県大佐山地域に産するフェロ藍閃石片岩
- Heavy mineral analysis of alluvial aedinents from the Akwatia area of the Birim diamonndierous field, Ghana
- 西南日本の地殻及び上部マントルの三次元P波速度構造