島根大学地球資源環境学研究報告

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島根大学地球資源環境学研究報告 13
1994-11-30 発行

飯梨川デルタのボーリング資料から見た地下構造

Subsurface geometry of the Iinashi Delta, Yasugi City, Shimane Prefecture
増井 貴
和田 直美
佐藤 勉
ファイル
内容記述(抄録等)
The Subsurface geometry of the Iinashi Delta,has been determined drilling data.Prodelta muddy sediments(Nakaumi Formation)about 20m thick,are overlain by,a 10m-thick deltaic sandy sequence.The delta sequence in the river mouth area is divided into a lower sandy layer(<10m),a middle sandy mud layer(8m),and an upper from sandy layer(10~15m).The lower and upper sandy lsyers are easily differentiated,each other by their sedimentary features.The middle sandy mud layer is developed only in the frontal part,and is inferred to have been deposited during the Heian Transgression at 1,200Y.B.P.
DOI(SelfDOI)