Traces of tsunami preserved in inter-tidal lacustrine and marsh deposits: some examples from northeast Japan

K. Minoura; S. Nakaya

doi:10.1086/629488

Traces of tsunami preserved in inter-tidal lacustrine and marsh deposits: some examples from northeast Japan

K. Minoura, S. Nakaya

SCI - Earth Science

Research output: Contribution to journal › Article › peer-review

274 Citations (Scopus)

Abstract

The Japan Sea Earthquake of May 26, 1983 triggered a large-scale tsunami that surged over the coast of NE Japan and caused considerable damage. The tsunami resulted in peculiar sedimentary processes on the coast. Depending on the hydraulic scale of the tsunami, three kinds of sedimentary processes were recognized, each of which left unique deposits. Such deposits are expected to remain in sedimentary sequences, preserving remarkable sedimentary facies. -from Authors

Original language	English
Pages (from-to)	265-287
Number of pages	23
Journal	Journal of Geology
Volume	99
Issue number	2
DOIs	https://doi.org/10.1086/629488
Publication status	Published - 1991 Jan 1

ASJC Scopus subject areas

Geology

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10.1086/629488

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abstract = "The Japan Sea Earthquake of May 26, 1983 triggered a large-scale tsunami that surged over the coast of NE Japan and caused considerable damage. The tsunami resulted in peculiar sedimentary processes on the coast. Depending on the hydraulic scale of the tsunami, three kinds of sedimentary processes were recognized, each of which left unique deposits. Such deposits are expected to remain in sedimentary sequences, preserving remarkable sedimentary facies. -from Authors",

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N2 - The Japan Sea Earthquake of May 26, 1983 triggered a large-scale tsunami that surged over the coast of NE Japan and caused considerable damage. The tsunami resulted in peculiar sedimentary processes on the coast. Depending on the hydraulic scale of the tsunami, three kinds of sedimentary processes were recognized, each of which left unique deposits. Such deposits are expected to remain in sedimentary sequences, preserving remarkable sedimentary facies. -from Authors

AB - The Japan Sea Earthquake of May 26, 1983 triggered a large-scale tsunami that surged over the coast of NE Japan and caused considerable damage. The tsunami resulted in peculiar sedimentary processes on the coast. Depending on the hydraulic scale of the tsunami, three kinds of sedimentary processes were recognized, each of which left unique deposits. Such deposits are expected to remain in sedimentary sequences, preserving remarkable sedimentary facies. -from Authors

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Traces of tsunami preserved in inter-tidal lacustrine and marsh deposits: some examples from northeast Japan

Abstract

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