{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360011142930002816.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.sedgeo.2012.07.019"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073812002096?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0037073812002096?httpAccept=text/plain"}}],"dc:title":[{"@value":"Sediment sources and sedimentation processes of 2011 Tohoku-oki tsunami deposits on the Sendai Plain, Japan — Insights from diatoms, nannoliths and grain size distribution"}],"description":[{"notation":[{"@value":"Abstract   The 11th March 2011 Tohoku-oki tsunami inundated the low-lying Sendai Plain (Japan) more than 5 km inland leaving sand and mud deposits over most of the area. In order to establish the sources of the tsunami deposits and interpret processes of their sedimentation, samples were collected from the deposits, underlying soils and the beach along a shore-perpendicular transect and analysed for grain size, diatom assemblages and nannoliths. The fining-inland tsunami deposits consisted of poorly to moderately sorted medium to coarse sand within 2 km of the coastline and very poorly to poorly sorted mud farther inland. More specifically, there was a slight fining of the coarse to medium sand mode within the sandy deposits and an increased contribution of the coarse and very coarse silt fraction in the mud deposits. The tsunami deposits also exhibited vertical changes including fining upward and coupled coarsening-fining upward trends. Few diatoms were present in beach sediments, soils and tsunami deposits within 1 km of the coastline, while diatoms were more abundant farther inland. Diatom assemblages in the soil and tsunami deposits were similar and dominated by species typical of freshwater-brackish habitats, while no typically marine species were encountered. Nannoliths were generally absent in the studied sediments, except for few specimens. Our data indicate that there was probably no or only a very minor component of marine sediments transported onland by the tsunami. The sandy tsunami deposits within ~ 1 km of the coastline were mostly derived from beach and dune erosion. From 1 to 2 km landward the contribution of these sources decreased, while sources comprising local soil erosion and the entrainment of sediments from the Teizan-bori canal increased. Farther inland, local soil erosion was the major sediment source for the mud deposits. The tsunami deposits were most likely deposited during at least two inundations, mostly out from suspension resulting in an upward grain size fining trend. However, bed load deposition was also important in the sandy deposits as suggested by a common grain size upward coarsening, position on C–M diagrams and frequent horizontal lamination. The present study reveals that even very large tsunamis may not transport marine sediments onland and thus many commonly applied indicators of tsunami deposits based on the assumption of their offshore origin (marine diatoms, foraminifera, nannoliths, marine sediments) may be of limited use."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011142930002820","@type":"Researcher","foaf:name":[{"@value":"Witold Szczuciński"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142930002819","@type":"Researcher","foaf:name":[{"@value":"Mikołaj Kokociński"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142930002821","@type":"Researcher","foaf:name":[{"@value":"Michał Rzeszewski"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142930002822","@type":"Researcher","foaf:name":[{"@value":"Catherine Chagué-Goff"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142930002816","@type":"Researcher","foaf:name":[{"@value":"Mario Cachão"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142930002817","@type":"Researcher","foaf:name":[{"@value":"Kazuhisa Goto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142930002818","@type":"Researcher","foaf:name":[{"@value":"Daisuke Sugawara"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00370738"}],"prism:publicationName":[{"@value":"Sedimentary Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-12","prism:volume":"282","prism:startingPage":"40","prism:endingPage":"56"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0037073812002096?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0037073812002096?httpAccept=text/plain"}],"createdAt":"2012-08-02","modifiedAt":"2025-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335852005760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inverse Tsunami Flow Modeling Including Nonequilibrium Sediment Transport, With Application to Deposits From the 2011 Tohoku-Oki Tsunami"},{"@value":"Inverse Tsunami Flow Modeling Including Nonequilibrium Sediment Transport, With Application to Deposits From the 2011 Tohoku‐Oki Tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001339198977664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological record of prehistoric tsunamis in Mugi town facing the Nankai Trough western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282813846346112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Examination of the largest-possible tsunamis (Level 2) generated along the Nankai and Suruga troughs during the past 4000years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"},{"@value":"Examination of the largest-possible tsunamis (Level 2 tsunami) generated along the Nankai and Suruga troughs during the past 4000 years based on studies of tsunami deposits from the 2011 Tohoku-oki tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215407748224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vertical distribution and formation analysis of the 131I, 137Cs, 129mTe, and 110mAg from the Fukushima Dai-ichi Nuclear Power Plant in the beach soil"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216157635200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological evidence and sediment transport modelling for the 1946 and 1960 tsunamis in Shinmachi, Hilo, Hawaii"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168825673856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Holocene coastal evolution, past tsunamis, and extreme wave event reconstructions using sediment cores obtained from the central coast of Hidaka, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870541779968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial Extent of Mid‐To Late‐Holocene Sedimentary Record of Tsunamis Along the Southern Kuril Trench, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690395977728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine biomarkers deposited on coastal land by the 2011 Tohoku-oki tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691040755584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Historical tsunami and storm deposits during the last five centuries on the Sanriku coast, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707329611648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical and micropaleontological impacts caused by the 2011 Tohoku-oki tsunami in Matsushima Bay, northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707474875520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami history over the past 2000 years on the Sanriku coast, Japan, determined using gravel deposits to estimate tsunami inundation behavior"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711655099264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Historical Nankai-Suruga megathrust earthquakes recorded by tsunami and terrestrial mass movement deposits on the Shirasuka coastal lowlands, Shizuoka Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617389993856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Holocene tsunami, storm, and relative sea level records obtained from the southern Hidaka coast, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298757436496640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fossil diatom assemblage changes due to paleoenvironment change, tsunami, and typhoon in southern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166017452672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial thickness variability of the 2011 Tohoku-oki tsunami deposits along the coastline of Sendai Bay"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168117724672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tsunami deposit associated with the 2011 Tohoku‐oki tsunami in the Hasunuma site of the Kujukuri coastal plain, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180532124800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Restoration Measures After the 2011 Tohoku-oki Tsunami and Their Impact on Tsunami Research"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182451575424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Are inundation limit and maximum extent of sand useful for differentiating tsunamis and storms? An example from sediment transport simulations on the Sendai Plain, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092710202240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ten years after the 2011 Tohoku-oki earthquake and tsunami: Geological and environmental effects and implications for disaster policy changes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118689414272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Identification of Coastal Sand Deposits From Tsunamis and Storm Waves Based on Numerical Computations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580230599303424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geological record of 18th and 19th century tsunamis along the Japan Sea coast of Tsugaru Peninsula, northwestern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339779761536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Understanding paleo-earthquakes in the Kuril Trench based on Late-Holocene tsunami deposits in the distal region from wave sources, northern Hidaka, Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657282987264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Erosion of a paleo-tsunami record by the 2011 Tohoku-oki tsunami along the southern Sendai Plain"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657399151616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoenvironments and relative sea-level changes caused by regional tectonics during the last 4500 years in Kumihama Bay, northern Kyoto Prefecture, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567450716160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A geochemical approach for identifying marine incursions: Implications for tsunami geology on the Pacific coast of northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567698318848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geochemical approaches in tsunami research: current knowledge and challenges"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865814752045824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Can Mud Deposits Indicate Inundation Extent of Paleotsunamis? Insights From Sediment‐Transport Simulations for Sand and Mud"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269875794560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Investigating beach erosion related with tsunami  sediment transport at Phra Thong Island, Thailand,  caused by the 2004 Indian Ocean tsunami"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204238331392","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"主成分分析を用いた次元圧縮に基づく東北地方太平洋沖地震による津波堆積物の地球化学的特性評価"},{"@language":"en","@value":"Evaluation of Geochemical Characteristics of Tsunami Deposits by the 2011 off the Pacific Cost of Tohoku Earthquake Using Dimensionality Reduction with a Principal Component Analysis"},{"@language":"ja-Kana","@value":"シュセイブン ブンセキ オ モチイタ ジゲン アッシュク ニ モトズク トウホク チホウ タイヘイヨウオキ ジシン ニ ヨル ツナミ タイセキブツ ノ チキュウ カガクテキ トクセイ ヒョウカ"},{"@value":"Evaluation of geochemical characteristics of tsunami deposits by the 2011 earthquake off the Pacific Coast of Tohoku using dimensionality reduction with a principal component analysis [in Japanese with English abstract]"},{"@value":"Evaluation of geochemical characteristics of tsunami deposits by the 2011 off the pacific cost of tohoku earthquake using dimensionality reduction with a principal component analysis. (in Japanese with English Abstract)"},{"@value":"Evaluation of geochemical characteristics of tsunami deposits by the 2011 off the Pacific Coast of Tohoku Earthquake using dimensionally reduction with a principal component analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205218404992","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sedimentary characteristics of the onshore tsunami deposits formed by the 2011Tohoku-oki tsunami in coastal lowlands, Ibaraki and Chiba prefectures"},{"@language":"ja","@value":"2011年東北地方太平洋沖地震津波により茨城県・千葉県沿岸低地に形成された津波堆積物の堆積学的特徴"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240047616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami sedimentation and deposits due to the 2011 Tohoku earthquake:"},{"@language":"ja","@value":"2011年東北地方太平洋沖地震による津波の堆積作用と堆積物："},{"@value":"2011年東北地方太平洋沖地震による津波の堆積作用と堆積物 : 広田湾と仙台湾の事例を中心とする検討"},{"@language":"ja-Kana","@value":"2011ネン トウホク チホウ タイヘイヨウオキ ジシン ニ ヨル ツナミ ノ タイセキ サヨウ ト タイセキブツ : ヒロタワン ト センダイワン ノ ジレイ オ チュウシン ト スル ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288144425984","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Current progress and future perspectives of the research on tsunami deposits using flume experiments"},{"@language":"ja","@value":"水路実験による陸上津波堆積物研究の現状と今後の可能性"},{"@language":"ja-Kana","@value":"スイロ ジッケン ニ ヨル リクジョウ ツナミ タイセキブツ ケンキュウ ノ ゲンジョウ ト コンゴ ノ カノウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679215042048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Radiocarbon Dating Historical Tsunami Deposits from the Sendai Plain, Northeastern Japan: Preliminary Age Model of HS Continuous Soil Sediment Series"},{"@language":"ja","@value":"仙台平野における歴史津波堆積物の放射性炭素年代測定"},{"@value":"仙台平野における歴史津波堆積物の放射性炭素年代測定 : 連続土壌堆積物試料HSシリーズの堆積年代(予察的分析)"},{"@language":"ja-Kana","@value":"センダイ ヘイヤ ニ オケル レキシ ツナミ タイセキブツ ノ ホウシャセイ タンソ ネンダイ ソクテイ : レンゾク ドジョウ タイセキブツ シリョウ HS シリーズ ノ タイセキ ネンダイ(ヨサツテキ ブンセキ)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680196699776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"エスチュアリー埋積堆積物中の津波堆積物:福島県南相馬市小高区井田川地区における完新統ボーリングコア"},{"@language":"en","@value":"Tsunami deposits in the estuary-fill:Holocene drill core in Minamisoma City, Fukushima Prefecture, Northeast Japan"},{"@language":"ja-Kana","@value":"エスチュアリーマイセキ タイセキブツ チュウ ノ ツナミ タイセキブツ : フクシマケン ミナミソウマシ コダカク イダガワ チク ニ オケル カンシントウボーリングコア"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217857792","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inundation areas and deposits of the 2011 off the Pacific coast of Tohoku and the 869 Jogan Earthquake Tsunamis"},{"@language":"ja","@value":"2011年東北地方太平洋沖地震津波と869年貞観地震津波の浸水域と堆積物"},{"@value":"Inundation areas and deposits of the 2011 of the pacific coast of Tohoku and the 869 Jogan earthquake tsunami. (2011-nen Tohoku-chihou Taiheiyouoki-Jishin tsunami to 869-nen Jyokan-Jishin tsunami no Shinsuiiki to Taisekibutsu)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390291115030290816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Event deposits recognized in the lowlands along the Tsugaru Strait, Hokkaido, Japan"},{"@language":"ja","@value":"北海道津軽海峡沿岸域で認められたイベント堆積物"}]},{"@id":"https://cir.nii.ac.jp/crid/1390579599231496320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimating Layer Boundaries of Mixed-layer Tsunami Deposits with a XRF Core Scanner"},{"@language":"ja","@value":"XRFコアスキャナーを用いた混合層中の津波堆積物の層境界の推定"},{"@language":"ja-Kana","@value":"XRF コアスキャナー オ モチイタ コンゴウソウ チュウ ノ ツナミ タイセキブツ ノ ソウ キョウカイ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390579599231498752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simple and Rapid Method for Geochemically Discriminating of Paleotsunami Deposits Using a Portable X-ray Fluorescence Spectrometry System: Application to Boring Cores from the Shizuoka Plain on the Pacific Coast of Central Japan"},{"@language":"ja","@value":"ポータブル蛍光エックス線分析装置による津波堆積物の簡易判別手法の検討"},{"@value":"ポータブル蛍光エックス線分析装置による津波堆積物の簡易判別手法の検討 : 静岡平野から採取したボーリングコア試料への適用"},{"@language":"ja-Kana","@value":"ポータブル ケイコウ エックスセン ブンセキ ソウチ ニ ヨル ツナミ タイセキブツ ノ カンイ ハンベツ シュホウ ノ ケントウ : シズオカ ヘイヤ カラ サイシュ シタ ボーリングコア シリョウ エ ノ テキヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390860332468668416","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of the 2011 Muddy and Organic-rich Tsunami Deposits in the Tohoku Region: An Overview"},{"@language":"ja","@value":"2011年東北沖津波の泥質・有機質津波堆積物"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417112339200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Using molluscan assemblages from paleotsunami deposits to evaluate the influence of topography on the magnitude of late Holocene mega-tsunamis on Ishigaki Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792001117440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial distribution and sources of tsunami deposits in a narrow valley setting - 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