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Estimating Layer Boundaries of Mixed-layer Tsunami Deposits with a XRF Core Scanner

Dados Bibliográficos

ID21348841
AutoresKengo Nakamura (0000-0002-2304-1548, Tohoku University), Tatsu KUWATANI (0000-0001-7161-9458, Research Institute for Marine Geodynamics, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)), Takeshi Komai (0000-0003-2244-5177, Tohoku University)
Ano2023
Volume132
Fascículo5
Páginas403-415
Data de publicação2023-10-25
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoJournal of Geography (Chigaku Zasshi) (JOURNAL)
Identificadores do periódicoISSN: 0022-135X • E-ISSN: 1884-0884
EditoraTokyo Geographical Society (PUBLISHER • JP)
DOI10.5026/jgeography.132.403
OpenAlexW4388558047
IdiomaEN
Citações recebidas5
Referências citadas31

From the perspective of disaster prevention, it is necessary to clarify the distribution and historical frequency of tsunami deposits. However, tsunami deposits are disturbed by earthquakes and tsunamis. Therefore, it is difficult to identify the layers of deposits. Layers deposited during disturbances are dated and grain-size distribution is measured. Using the results of geochemical data and principal component analyses with detailed elemental distributions, stratigraphic boundaries of past tsunami deposit layers and other layers left in the disturbed deposits are estimated. Samples collected with a geo-slicer consist of a 50-60 cm deep disturbed layer deposited by the Great East Japan Earthquake and underlying sand, peat, and marine deposits. 24 elemental distributions in a core measured using Itrax indicate that the disturbed layer is dominated by heavy metals. Changes in principal component analysis scores infer traces of a layer that could not be visually identified in the disturbed layer. Traces of this layer are consistent with traces that are deposits indicated from the isotopic analysis and the grain size distribution. Therefore, even if it is difficult to identify deposits due to disturbances caused by the tsunami, it may be possible to identify unidentified layers and estimate their thicknesses by compressing their dimensions and clarifying elemental relationships

Core (optical fiber) · Geochemistry · Layer (electronics) · Mineralogy · Principal component analysis · earthquake and tectonic studies · Geological and Geochemical Analysis · Geology · Geology and Paleoclimatology Research · Materials Science

  • Overview of the Special Issue “Progress of Earth and Data Sciences Research into Tsunami Deposits, and Contribution to Tsunami Disaster Prevention (Part I)

    Open Access•Noriyoshi Tsuchiya, Takeshi Komai et al.•Journal of Geography (Chigaku…•2023

  • Preface of the Special Issue “Progress of Earth and Data Sciences Research into Tsunami Deposits, and Contribution to Tsunami Disaster Prevention (Part I)

    Open Access•Noriyoshi Tsuchiya, Takeshi Komai et al.•Journal of Geography (Chigaku…•2023

  • Preface of the Special Issue “Progress of Earth and Data Sciences Research into Tsunami Deposits, and Contribution to Tsunami Disaster Prevention (Part II)

    Open Access•Noriyoshi Tsuchiya, Takeshi Komai et al.•Journal of Geography (Chigaku…•2023

  • Overview of the Special Issue “Progress of Earth and Data Sciences Research into Tsunami Deposits, and Contribution to Tsunami Disaster Prevention (Part II)

    Open Access•Noriyoshi Tsuchiya, Takeshi Komai et al.•Journal of Geography (Chigaku…•2023

  • Statistical Correlation for Geological Layers Using XRF Core Scan Data

    Open Access•Tatsu KUWATANI, Toshimoto SAKAI et al.•Journal of Geography (Chigaku…•2023

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    Open Access•Ludvig Löwemark, Menno Bloemsma et al.•Quaternary International•2019

  • Marine incursions of the past 1500 years and evidence of tsunamis at Suijin-numa, a coastal lake facing the Japan Trench

    Open Access•Yuki Sawai, Yushiro Fujii et al.•The Holocene•2008

  • IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP

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Obras citantes distintas5
Citações por ano1,67
Intervalo de citações2023 - 2023 (1)
Velocidade de citaçãohistorical
Altamente citadoNão
Tipos de citaçãoNeutras: 5
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