{"@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/1360846643404863744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1130/g32043.1"}},{"identifier":{"@type":"NAID","@value":"10030744591"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Episodic seafloor mud brecciation due to great subduction zone earthquakes"}],"description":[{"notation":[{"@value":"The Nankai Trough off southwest Japan has an ∼1300 yr historical record of great earthquakes, including the most recent, the A.D. 1944 Tonankai (M = 8.2) earthquake. Evaluation of the activity of an individual submarine fault is difficult when only onland observations are available. Submarine core records can pinpoint individual fault activity. Here we present Integrated Ocean Drilling Program (IODP) Nankai Trough Seismogenic Zone Experiment data from the shallow portion. IODP Expedition 316 drilled and cored several holes in the shallow portion of the offshore Tonankai earthquake area, including sites in the hanging wall of a margin-dominating splay fault that has previously been interpreted to have ruptured coseismically during megathrust earthquakes. X-ray computed tomography scanning revealed that the uppermost core at one site contains repeated occurrences of mud breccia. Radioisotope dating of the uppermost mud breccia indicates a deposition time consistent with the 1944 Tonankai earthquake, suggesting that the mud-breccia layers result from episodic brecciation caused by seismic shaking. Mud brecciation provides a potential new tool to reconstruct ancient earthquake history in subduction zones."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1581135650774639104","@type":"Researcher","foaf:name":[{"@value":"A. Sakaguchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847871642144005","@type":"Researcher","foaf:name":[{"@value":"G. Kimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847871642144001","@type":"Researcher","foaf:name":[{"@value":"M. Strasser"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847871642144002","@type":"Researcher","foaf:name":[{"@value":"E. J. Screaton"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847871642144003","@type":"Researcher","foaf:name":[{"@value":"D. Curewitz"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847871642144000","@type":"Researcher","foaf:name":[{"@value":"M. Murayama"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00917613"},{"@type":"EISSN","@value":"19432682"}],"prism:publicationName":[{"@value":"Geology"}],"dc:publisher":[{"@value":"Geological Society of America"}],"prism:publicationDate":"2011-09-02","prism:volume":"39","prism:number":"10","prism:startingPage":"919","prism:endingPage":"922"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","createdAt":"2011-09-13","modifiedAt":"2023-06-09","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782144521216","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23244099"},{"@type":"JGN","@value":"JP23244099"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23244099/"}],"notation":[{"@language":"ja","@value":"沈み込み地震発生分岐断層の断層メカニズムとその進化"},{"@language":"en","@value":"Fault mechanism and evolution of the seismogenic splay fault in subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257039322624","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21107003"},{"@type":"JGN","@value":"JP21107003"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21107003/"}],"notation":[{"@language":"ja","@value":"高精度変動地形・地質調査による巨大地震断層の活動履歴の解明"},{"@language":"en","@value":"High precision topographical/geological surveys for elucidating the activity history of seismogenic faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257039342080","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21107005"},{"@type":"JGN","@value":"JP21107005"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21107005/"}],"notation":[{"@language":"ja","@value":"巨大地震断層の物質科学的研究によるすべりメカニズムの解明"},{"@language":"en","@value":"Materials and slip processes of seismogenic faults"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202652261888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Vein structures like ripple marks are formed by short-wavelength shear waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001335780632192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Characteristics of a tsunamigenic megasplay fault in the Nankai Trough"}]},{"@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/1050845760779256704","@type":"Article","resourceType":"学術雑誌論文(journal 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sample"}]},{"@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/1360292617916830848","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619658479744","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Accretion, mass wasting, and partitioned strain over the 26 Dec 2004 Mw9.2 rupture offshore Aceh, northern Sumatra"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165846900352","@type":"Article","resourceType":"学術雑誌論文(journal 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earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360579820492765952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Major earthquakes in Mexicali Valley, Mexico, and fluid extraction at Cerro Prieto Geothermal Field"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453482368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contrasting hydrological and mechanical properties of clayey and silty muds cored from the shallow Nankai Trough accretionary prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568869599616","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics of amplitude and duration for near fault strong ground motion from the 1999 Chi-Chi, Taiwan Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043442520448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bottom response to a tsunami earthquake: Submersible observations in the epicenter area of the 1993 earthquake off southwestern Hokkaido, Sea of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043907937664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coastal sedimentation associated with the December 12th, 1992 tsunami in Flores, Indonesia"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995123926016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Mechanical development of vein structures due to the passage of earthquake waves through poorly-consolidated sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995252579072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rupture process of the 1944 Tonankai earthquake (<i>M</i><sub><i>s</i></sub> 8.1) from the inversion of teleseismic and regional seismograms"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468767487104","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantitative analysis of seismogenic shear-induced turbulence in lake sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981471341518080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Soft sediment deformation by Kelvin Helmholtz Instability: A case from Dead Sea earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944450966272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleoseismicity along the southern Kuril Trench deduced from submarine-fan turbidites"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418498574336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismological monitoring on the 2003 Tokachi-oki earthquake, derived from off Kushiro permanent cabled OBSs and land-based observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369249416960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Northwest Pacific Marine Reservoir Correction Estimated from Annually Banded Coral from Ishigaki Island, Southern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369579241984","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Increased marine sediment suspension and fluxes following an earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388843831355392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trampoline Effect in Extreme Ground Motion"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844326141312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A 1,000-year sediment record of tsunami recurrence in northern 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State"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233271177369088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Holocene Earthquake Records from the Cascadia Subduction Zone and Northern San Andreas Fault Based on Precise Dating of Offshore Turbidites"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204552173824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Methane production and accumulation in the Nankai accretionary prism: Results from IODP Expeditions 315 and 316"},{"@value":"Gas Chemistry of Pore Fluids from Oomine Ridge on the Nankai Accretionary Prism"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205218749696","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Perspectives of sedimentological analysis in riser drilling expeditions"},{"@language":"ja","@value":"ライザー掘削航海で望まれる新たな堆積学的分析手法"},{"@language":"ja-Kana","@value":"ライザー クッサク コウカイ デ ノゾマレル アラタ ナ タイセキガクテキ ブンセキ シュホウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241273088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Identification of a Soil Liquefied Layer due to the 2011 off the Pacfic coast of Tohoku Earthquake Using X-ray CT Scan Imaging:"},{"@language":"ja","@value":"ボーリングコアのX線CTスキャン解析による東北地方太平洋沖地震における地盤液状化層の同定："},{"@value":"ボーリングコアのX線CTスキャン解析による東北地方太平洋沖地震における地盤液状化層の同定 : 浦安市舞浜3丁目コア試料の例"},{"@language":"ja-Kana","@value":"ボーリングコア ノ Xセン CT スキャン カイセキ ニ ヨル トウホク チホウ タイヘイヨウオキ ジシン ニ オケル ジバン エキジョウカソウ ノ ドウテイ : ウラヤスシ マイハマ 3チョウメ コア シリョウ ノ レイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513406976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source rupture processes of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low-gain seismograms"},{"@value":"Source rupture process of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low‐gain seismograms"},{"@value":"Source rupture process of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low-gain seismograms"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679039868416","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Value of X-ray computed tomography in the scientific ocean drilling"},{"@language":"ja","@value":"科学海洋掘削におけるX線断層撮影法の有効性の評価"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679214776064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fault-Drilling Investigation of Earthquake Slip Behavior and Physicochemical Processes"},{"@language":"ja","@value":"断層掘削研究によって明らかになった地震時の断層滑り挙動とその物理化学的側面"},{"@language":"ja-Kana","@value":"ダンソウ クッサク ケンキュウ ニ ヨッテ アキラカ ニ ナッタ ジシンジ ノ ダンソウ スベリ キョドウ ト ソノ ブツリ カガクテキ ソクメン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681474009216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"ターミナル小海盆：タービダイト古地震学の一つのターゲット"},{"@language":"en","@value":"Terminal basin as a target for turbidite paleoseismology"},{"@value":"2014年日本第四紀学会学術賞受賞記念論文 ターミナル小海盆 : タービダイト古地震学の一つのターゲット"},{"@language":"ja-Kana","@value":"2014ネン ニホン ダイシキ ガッカイ ガクジュツショウ ジュショウ キネン ロンブン ターミナル コウミボン : タービダイト コ ジシンガク ノ ヒトツ ノ ターゲット"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238023962752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"海底の地震・津波堆積物"},{"@language":"en","@value":"Submarine earthquake– and tsunami–induced event 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