2024-03-29T09:42:51Z
https://soar-ir.repo.nii.ac.jp/oai
oai:soar-ir.repo.nii.ac.jp:00012067
2023-03-08T01:52:12Z
1169:1171:1172:1190
波浪卓越沿岸の堆積相 : 北部フォッサマグナ中期中新世の礫質堆積物から
Sedimentary fades and environment of the Middle Miocene coarse-grained and storm dominated coastal sediments in the Northern Fossa Magna region
西村, 瑞恵
渡辺, 大輔
保柳, 康一
As wave pass across the shallowing profile of the shelf to beach face they interact with the sediment surface and transformed, producing a series of hydrodynamic zones aligned approximately parallel to the shoreline. The sedimentary facies is determined for each hydrodynamic zone. We propose the sedimentary facies model for storm dominated shelf which is illustrated from the Middle Miocene coarse-grained sedimentary rocks in Northern Fossa Magna region. These sedimentary facies considered to have been distributed in the margin of a fan delta system, where the coarse grained sediments are mainly transported by wave and nearshore currents.
Article
信州大学理学部紀要 29(2): 71-77(1995)
信州大学理学部
1995-03-30
jpn
departmental bulletin paper
VoR
http://hdl.handle.net/10091/10624
https://soar-ir.repo.nii.ac.jp/records/12067
0583-063X
AA00697923
信州大学理学部紀要
29
2
71
77
https://soar-ir.repo.nii.ac.jp/record/12067/files/Science29-02-02.pdf
application/pdf
945.8 kB
2015-09-28