Geoscience reports of Shimane University

島根大学総合理工学部地球資源環境学教室

ISSN:1343-9774

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Use this link to cite this item : https://ir.lib.shimane-u.ac.jp/6101

Geoscience reports of Shimane University 20

2001-12-28 発行

弓ヶ浜砂州の地下地質

Late Quaternary sediments of the Yumigahama sandbar,Tottori Prefecture,Southwest Japan

Nakamura, Tadashi

Shigematsu, Shinji

Tokuoka, Takao

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c006020023.pdf 1.35 MB

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The subsurface geology of the Yumigahama sandbar has been reconstructed mainly on the basis of drilling data from 15 drillcores put down by the Ministry of Construction in 1995～1996．The sandbar is underlain by layers of Holocene sand，Holocene mud and Pleistocene sand，in descending order. Two volcanic ash layers，the SKP（Sanbe-Kisuki Pumice）and the DMP（Daisen-Matsue Pumice）are intercalated in upper part of the Pleistocene deposits，and the K-Ah volcanic ash layer（6,300 yr B.P.）is intercalated in the muddy Holocene deposits．

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c006020023.pdf 1.35 MB

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