{"@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/1360004232523299840.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.tecto.2011.03.002"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195111000849?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195111000849?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Rheological structure of northeastern Japan lithosphere based on geophysical observations and rock mechanics"}],"description":[{"notation":[{"@value":"Abstract   Based on recent results on rock mechanics and geophysical observations, I constructed rheological (strength and viscosity) profiles across the northeastern Japan lithosphere. The profiles well explain patterns of present-day geodetic strain accumulation and shallow seismicity. Experimentally derived flow laws also predict the presence of weak zones by mechanisms likely operated in the lithosphere (e.g., partial melting and shear zone development). The strain localization into weak zones explains the estimates of low viscosity (1019–1020 Pas) from post-seismic creep after a large inland earthquake. The strain localization into weak zones also efficiently accumulates elastic strains at the base of upper seismogenic faults locked during interseismic periods resulting in the reactivation of pre-existing fault systems in the northeastern Japan."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751139829120","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40545787"},{"@type":"NRID","@value":"1000040545787"},{"@type":"ORCID","@value":"0000-0001-8493-4051"},{"@type":"NRID","@value":"9000290384773"},{"@type":"NRID","@value":"9000003543833"},{"@type":"NRID","@value":"9000238256265"},{"@type":"NRID","@value":"9000386338253"},{"@type":"NRID","@value":"9000406036887"},{"@type":"NRID","@value":"9000001768651"},{"@type":"NRID","@value":"9000398987557"},{"@type":"NRID","@value":"9000409997294"},{"@type":"NRID","@value":"9000332226140"},{"@type":"NRID","@value":"9000405103790"},{"@type":"NRID","@value":"9000398037244"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/junmuto"}],"foaf:name":[{"@value":"Jun Muto"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2011-04","prism:volume":"503","prism:number":"3-4","prism:startingPage":"201","prism:endingPage":"206"},"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:S0040195111000849?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195111000849?httpAccept=text/plain"}],"createdAt":"2011-03-16","modifiedAt":"2025-09-22","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257110836736","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22740328"},{"@type":"JGN","@value":"JP22740328"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22740328/"}],"notation":[{"@language":"ja","@value":"下部地殻部分溶融体のレオロジーと弾性波速度に関する実験的研究"},{"@language":"en","@value":"Experimental research on rheology and seismic wave velocity properties of partially molten lower crustal rocks"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202726471680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional structure of V_p, V_s, and V_p/V_s beneath northeastern Japan: Implications for arc magmatism and fluids"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001202746187008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimation of thermal structure in the mantle wedge of northeastern Japan from seismic attenuation data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050025031479798400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strain anomalies induced by the 2011 Tohoku Earthquake (Mw 9.0) as observed by a dense GPS network in northeastern Japan"},{"@value":"Strain anomalies induced by the 2011 Tohoku Earthquake ("}]},{"@id":"https://cir.nii.ac.jp/crid/1050585039689055744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Low-temperature, high-stress deformation of olivine under water-saturated conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230122316544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two‐dimensional viscosity structure of the northeastern Japan islands arc‐trench system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523450368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Method for correction of differential stress calculations from experiments using the solid salt assembly in a Griggs-type deformation apparatus"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143727795584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rheology of fine-grained siliciclastic rocks in the middle crust—evidence from structural and numerical analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144640539776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rheology of the lithosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011146070699008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simultaneous high P‐T measurements of ultrasonic compressional and shear wave velocities in Ichino‐megata mafic xenoliths: Their bearings on seismic velocity perturbations in lower crust of northeast Japan arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429412596608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Inferring 3‐D Rheology of Low‐Viscosity Zone Around Quaternary Volcanoes of NE Japan From Postseismic Deformation of the 2011 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620467275136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rupturing in overpressured crust during compressional inversion—the case from NE Honshu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620560594816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fault zone fabric and fault weakness"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757965312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous stress state of island arc crust in northeastern Japan affected by hot mantle fingers"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180316129664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological Structure Beneath NE Japan Inferred from Coseismic Strain Anomalies Associated with the 2011 Tohoku-oki Earthquake (Mw9.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118713913600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Enhancement of ductile deformation in polycrystalline anorthite due to the addition of water"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569344746112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The solid‐state flow of polymineralic rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570484667520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evidence for dominant grain-boundary sliding deformation in greenschist- and amphibolite-grade polymineralic ultramylonites from the Redbank Deformed Zone, Central Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570878253952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Strength of the lithosphere: Constraints imposed by laboratory experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571286824576","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707157648384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-arc heterogeneous rheology inferred from post-seismic deformation of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707375192320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slab-derived fluid storage in the crust elucidated by earthquake swarm"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521130347904","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Plagioclase preferred orientation in layered mylonites: Evaluation of flow laws for the lower crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993396359552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Effects of pressure on high-temperature dislocation creep in olivine"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994109308544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Faulting processes controlled by the nonuniform thermal structure of the crust and uppermost mantle beneath the northeastern Japanese island arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469006700928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simulation of postseismic deformations caused by the 1896 Riku‐u Earthquake, northeast Japan: Re‐evaluation of the viscosity in the upper mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470748514944","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Laboratory measurement of P-wave velocity in crustal and upper mantle xenoliths from Ichino-megata, NE Japan: ultrabasic hydrous lower crust beneath the NE Honshu arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943650429568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The petrologic case for a dry lower crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944158865920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extensional structure in Northern Honshu Arc as inferred from seismic refraction/wide‐angle reflection profiling"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262944447488896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lithospheric loading by the 1896 Riku‐u Earthquake, northern Japan: Implications for plate flexure and asthenospheric rheology"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945447580160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Magnetotelluric imaging of fluids in intraplate earthquake zones, NE Japan Back Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420853601280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Experimental intracrystalline plastic flow in hot-pressed synthetic quartzite prepared from Brazilian quartz crystals"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895110516736","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep roots of upper plate faults and earthquake generation illuminated by volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895551106688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Grain size evolution and the rheology of ductile shear zones: from laboratory experiments to postseismic creep"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368867931008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep structure of the northeastern Japan arc and its implications for crustal deformation and shallow seismic activity"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844569174912","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional attenuation structure beneath the northeastern Japan arc estimated from spectra of small earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844653150464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Reaction-enhanced ductility: The role of solid-solid univariant reactions in deformation of the crust and mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845253618176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep seismic reflection profiling across the Ou Backbone range, northern Honshu Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845471065856","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Flow laws for rocks containing two non-linear viscous phases: A phenomenological approach"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318371830656","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Influence of water fugacity and activation volume on the flow properties of fine‐grained anorthite aggregates"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321265013376","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High‐temperature creep of partially molten plagioclase aggregates"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951793534061568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Frictional-viscous flow of simulated fault gouge caused by the combined effects of phyllosilicates and pressure solution"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795361353344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An episode of fault-valve behaviour during compressional inversion? — The 2004 MJ6.8 Mid-Niigata Prefecture, Japan, earthquake sequence"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951796196315008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stress and temperature in the bending lithosphere as constrained by experimental rock mechanics"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006144133810441","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geothermal gradient data in and around Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006144133810565","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deformation of earth materials"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240339712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rheological profile across the northeastern Japan lithosphere toward precise modeling of the 2011 Tohoku Oki Earthquake"},{"@language":"ja","@value":"東日本太平洋沖地震後の余効変動解析へ向けた東北日本弧レオロジー断面"},{"@language":"ja-Kana","@value":"ヒガシニホン タイヘイヨウオキ ジシン ゴ ノ ヨコウヘンドウ カイセキ エ ムケタ トウホク ニホン コ レオロジー ダンメン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490856192","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strain concentration zone along the volcanic front derived by GPS observations in NE Japan arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564227346651904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Flow of Lower Crust and Upper Mantle Inferred from Geological and Geophysical Observations"},{"@language":"ja","@value":"地質学的観察および測地学的観測から知る下部地殻・上部マントルの流動"},{"@language":"ja-Kana","@value":"チシツガクテキ カンサツ オヨビ ソクチガクテキ カンソク カラ シル カブ チカク ・ ジョウブ マントル ノ リュウドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390870529360676096","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北沖地震の余効変動から知る東北日本弧地殻マントルのレオロジー特性"},{"@language":"en","@value":"Rheological Properties of the Crust and Upper Mantle in Northeast Japan Following Postseismic Deformation from the 2011 Tohoku-oki Earthquake"},{"@value":"東北沖地震の余効変動から知る東北日本孤地殻マントルのレオロジー特性"},{"@language":"ja-Kana","@value":"トウホクオキ ジシン ノ ヨコウヘンドウ カラ シル トウホク ニホンコチカク マントル ノ レオロジー トクセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942184938624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic evidence of viscoelastic relaxation after the 2008 Iwate-Miyagi Nairiku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842066368640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267021825664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep structure of the Ou mountain range strain concentration zone and the focal area of the 2008 Iwate-Miyagi Nairiku earthquake, NE Japan : seismogenesis related with magma and crustal fluid"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.tecto.2011.03.002"},{"@type":"KAKEN","@value":"PRODUCT-13680342"},{"@type":"OPENAIRE","@value":"doi_dedup___::8356ec64832371b73e9192625fe2d13e"},{"@type":"CROSSREF","@value":"10.1002/grl.50906_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.5047/eps.2012.04.001_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0026_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1029/2024jb029939_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.5026/jgeography.135.61_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1002/2015jb012664_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1007/1345_2015_135_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.5047/eps.2012.05.015_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2022.104547_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1186/s40645-023-00539-1_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.02.011_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac063_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.1038/s43247-022-00610-7_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"},{"@type":"CROSSREF","@value":"10.5026/jgeography.128.731_references_DOI_BIfzEYnrdN39CWnuWEl2MCVRWob"}]}