{"@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/1361137046401267328.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2005jb004205"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005JB004205"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005JB004205"}},{"identifier":{"@type":"NAID","@value":"10028199433"}}],"dc:title":[{"@value":"Origin and mechanical significance of foliated cataclastic rocks in the cores of crustal‐scale faults: Examples from the Median Tectonic Line, Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The Median Tectonic Line (MTL) is Japan's largest onshore fault and has been active since the mid‐Cretaceous. Foliated cataclastic fault rocks are exceptionally well exposed in the fault core at Anko, Nagano Prefecture. Following an early phase of mylonitization and exhumation during left‐lateral shearing, brittle fracture and cataclasis occurred leading to the development of centimeter‐ to submillimeter‐spaced, fault zone parallel fracture systems. These fracture systems established an initial architectural hierarchy that influenced the subsequent development of foliated cataclasites and gouge. Initially, fracture systems coalesced to form interconnected zones of fine‐grained ultracataclasite. Fluid influx at the onset of grain‐scale brittle deformation led to precipitation of fibrous chlorite within the ultracataclasites, ultimately leading to the development of an interconnected network of foliated, phyllosilicate‐rich cataclasites and gouges in the core of the MTL. The brittle reduction of grain size and ingress of a chemically active fluid phase simultaneously promoted reaction softening and diffusive mass transfer in the foliated ultracataclasites, leading to rate‐dependent “frictional‐viscous” flow at sub‐Byerlee friction values. Associated weakening is indicated by the preferential localization of deformation within the ultracataclasites. A protracted sequence of carbonate mineralization and cementation events is also recognized during the fault rock evolution and suggests episodic periods of fluid overpressuring. A crustal‐scale fault zone model is proposed, suggesting that the foliated cataclasites/gouges are weak in the long term and represent shallower crustal equivalents of phyllonitic fault rocks exposed in more deeply exhumed fault zones, including other parts of the MTL.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1580854175853580928","@type":"Researcher","foaf:name":[{"@value":"S. P. Jefferies"}],"jpcoar:affiliationName":[{"@value":"Reactivation Research Group, Department of Earth Sciences University of Durham  Durham England, UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046401267329","@type":"Researcher","foaf:name":[{"@value":"R. E. Holdsworth"}],"jpcoar:affiliationName":[{"@value":"Reactivation Research Group, Department of Earth Sciences University of Durham  Durham England, UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046401267332","@type":"Researcher","foaf:name":[{"@value":"T. Shimamoto"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Mineralogy, Graduate School of Science Kyoto University  Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046401267328","@type":"Researcher","foaf:name":[{"@value":"H. Takagi"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Science Waseda University  Shinjuku, Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046401267330","@type":"Researcher","foaf:name":[{"@value":"G. E. Lloyd"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences University of Leeds  Leeds UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046401267333","@type":"Researcher","foaf:name":[{"@value":"C. J. Spiers"}],"jpcoar:affiliationName":[{"@value":"HPT Laboratory, Department of Earth Sciences Utrecht University  Utrecht Netherlands"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2006-12","prism:volume":"111","prism:number":"B12","prism:startingPage":"B12303"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005JB004205"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005JB004205"}],"createdAt":"2006-12-15","modifiedAt":"2023-10-12","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Fault%20gouge","dc:title":"Fault gouge"},{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=Median%20Tectonic%20Line","dc:title":"Median Tectonic Line"},{"@id":"https://cir.nii.ac.jp/all?q=Weakening%20processes.","dc:title":"Weakening processes."},{"@id":"https://cir.nii.ac.jp/all?q=Foliated%20cataclasite","dc:title":"Foliated cataclasite"},{"@id":"https://cir.nii.ac.jp/all?q=Fault%20reactivation","dc:title":"Fault reactivation"},{"@id":"https://cir.nii.ac.jp/all?q=Geowetenschappen%20en%20aanverwante%20(milieu)wetenschappen","dc:title":"Geowetenschappen en aanverwante (milieu)wetenschappen"},{"@id":"https://cir.nii.ac.jp/all?q=Weakening%20processes","dc:title":"Weakening processes"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050303932805502336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Comminution-Induced Transient Frictional Behavior in Sheared Granular Halite"},{"@value":"Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235527970176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recognition of shear heating on a long‐lived major fault using Raman carbonaceous material thermometry: implications for strength and displacement history of the MTL, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166128856448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of the Median Tectonic Line fault zone, SW Japan, during exhumation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118795254400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recognition of broad thermal anomaly around the median tectonic line in central Kii peninsula, <scp>southwest</scp> Japan: Possible heat sources"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654733480064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress rotations and the long-term weakness of the Median Tectonic Line and the Rokko-Awaji Segment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453588608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Blackening of fault gouge by comminution and pyrolysis of carbonaceous materials during earthquake slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1390004222631008640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamic Earthquake Cycle Simulations Considering Changes in Dominant Deformation Mechanisms of a Fault Slip"},{"@language":"ja","@value":"断層滑りの支配的な変形機構の遷移を考慮に入れた動的地震サイクルシミュレーション"},{"@language":"ja-Kana","@value":"ダンソウ スベリ ノ シハイテキ ナ ヘンケイ キコウ ノ センイ オ コウリョ ニ イレタ ドウテキ ジシン サイクルシミュレーション"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213869824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crush zone structure in a compressional step:"},{"@language":"ja","@value":"圧縮性ステップにおける破砕帯の構造"},{"@value":"圧縮性ステップにおける破砕帯の構造--岐阜県飛騨市の跡津川断層西部の例"},{"@language":"ja-Kana","@value":"アッシュクセイ ステップ ニ オケル ハサイタイ ノ コウゾウ ギフケン ヒダシ ノ アトツガワ ダンソウ セイブ ノ レイ"},{"@value":"Crush zone structure in a compressional step: an example of the western part of the Atotsugawa Fault, Hida City, Gifu Prefecture of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238052793472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Architecture of onshore fault zones"},{"@language":"ja","@value":"陸域断層の内部構造"},{"@language":"ja-Kana","@value":"リクイキ ダンソウ ノ ナイブ コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1570572700876867968","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reconstructing the evolution of fault zone architecture : Field-based study of the core region of the Atera Fault, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892091270528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The architecture of long-lived fault zones : insights from microstructure and quartz lattice-preferred orientations in mylonites of the Median Tectonic Line, SW Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005jb004205"},{"@type":"CIA","@value":"10028199433"},{"@type":"OPENAIRE","@value":"doi_dedup___::889306b53f3809518bd19b9656ea9b21"},{"@type":"CROSSREF","@value":"10.1111/iar.12129_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0261-6_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.5575/geosoc.114.495_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.12.017_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.491_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.03.039_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.1111/iar.12440_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.1002/2014tc003600_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2018.0004_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"},{"@type":"CROSSREF","@value":"10.1029/2024gl109645_references_DOI_B5w5H0Cvg3240Hvk3ohJcE6SmDa"}]}