{"@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/1360011144094087552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1144/gsjgs.133.3.0191"}},{"identifier":{"@type":"URI","@value":"https://www.lyellcollection.org/doi/pdf/10.1144/gsjgs.133.3.0191"}},{"identifier":{"@type":"NAID","@value":"80013772000"}}],"dc:title":[{"@value":"Fault rocks and fault mechanisms"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Physical factors likely to affect the genesis of the various fault rocks—frictional properties, temperature, effective stress normal to the fault and differential stress—are examined in relation to the energy budget of fault zones, the main velocity modes of faulting and the type of faulting, whether thrust, wrench, or normal. In a conceptual model of a major fault zone cutting crystalline quartzo-feldspathic crust, a zone of elastico-frictional (EF) behaviour generating random-fabric fault rocks (gouge—breccia—cataclasite series—pseudotachylyte) overlies a region where quasi-plastic (QP) processes of rock deformation operate in ductile shear zones with the production of mylonite series rocks possessing strong tectonite fabrics. In some cases, fault rocks developed by transient seismic faulting can be distinguished from those generated by slow aseismic shear. Random-fabric fault rocks may form as a result of seismic faulting within the ductile shear zones from time to time, but tend to be obliterated by continued shearing. Resistance to shear within the fault zone reaches a peak value (greatest for thrusts and least for normal faults) around the EF/QP transition level, which for normal geothermal gradients and an adequate supply of water, occurs at depths of 10–15 km.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1582261551371387520","@type":"Researcher","foaf:name":[{"@value":"R. H. SIBSON"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167649"},{"@type":"EISSN","@value":"2041479X"}],"prism:publicationName":[{"@value":"Journal of the Geological Society"}],"dc:publisher":[{"@value":"Geological Society of London"}],"prism:publicationDate":"1977-03","prism:volume":"133","prism:number":"3","prism:startingPage":"191","prism:endingPage":"213"},"reviewed":"false","dc:rights":["https://doi.org/10.15223/policy-002"],"url":[{"@id":"https://www.lyellcollection.org/doi/pdf/10.1144/gsjgs.133.3.0191"}],"createdAt":"2007-12-20","modifiedAt":"2024-11-19","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335764430080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repeated seismic slips recorded in ultracataclastic veins along active faults of the Arima–Takatsuki Tectonic Line, southwest Japan"},{"@value":"Repeated seismic slips recorded in 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分布および破砕-変質様式"},{"@language":"ja-Kana","@value":"ノジマ ダンソウ チシツ チョウサジョ コア ニ オケル ダンソウガン クブン ブンプ オヨビ ハサイ ヘンシツ ヨウシキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206233863424","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemistry of the Nihonkoku Mylonite along the border between Niigata and Yamagata Prefectures, Northeast Japan."},{"@language":"ja","@value":"新潟・山形県境に分布する日本国マイロナイトの地球化学"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206233864960","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Discovery of a mylonite Zone (Ringou Mylonite Zone) in Nanyo City, Yamagata Prefecture and the northern extension of the Tanagura Tectonic Line."},{"@value":"山形県南陽市周辺のマイロナイト帯（梨郷マイロナイト帯）の発見と棚倉構造線の北方延長問題"},{"@language":"ja-Kana","@value":"ヤマガタケン ナンヨウシ シュウヘン ノ マイロナイトタイ リンゴウ マイロナイトタイ ノ ハッケン ト タナグラ コウゾウセン ノ ホッポウ エンチョウ モンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206233939968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Intrusion of granitic magma and uplift tectonics of the Hidaka metamorphic belt, Hokkaido."},{"@value":"花こう岩質マグマのほう入と日高変成帯の衝上テクトニクス"},{"@language":"ja-Kana","@value":"カコウガンシツ マグマ ホウニュウ ト ヒダカ ヘンセイタイ ノ ショウジョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234022656","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar ages of the metamorphic and plutonic rocks in the southern part of the Hidaka belt, Hokkaido and their implications."},{"@language":"ja","@value":"北海道，日高帯南部における変成岩および深成岩のＫ‐Ａｒ年代とその意味"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234102784","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Web structure in the sandstone beds of the Emi Group in the southern part of the Boso Peninsula, central Japan."},{"@value":"房総半島南部江見層群砂岩層中に発達するｗｅｂ　ｓｔｒｕｃｔｕｒｅ"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ ナンブ エミソウグン サガンソウチュウ ニ ハッタツスル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234962176","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mylonite in the Ryoke metamorphic belt drilled at 100m away from the Median Tectonic Line, Misakubo, central Honshu, Japan."},{"@value":"静岡県水窪町で掘削されたマイロナイト柱状コアの変形構造解析　　中央構造線沿いの領家帯の地下構造と岩相境界への塑性せん断歪の局所化"},{"@language":"ja-Kana","@value":"シズオカケン ミサクボチョウ デ クッサク サレタ マイロナイト チュウジョウ コア ノ ヘンケイ コウゾウ カイセキ チュウオウ コウゾウセン ゾイ ノ リョウケタイ ノ チカ コウゾウ ト ガンソウ キョウカイ エ ノ ソセイセンダンワイ ノ キョクショカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234977280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy, geologic structures, and K-Ar ages of the Ryuhozan metamorphic rocks in western Kyushu, Japan."},{"@value":"九州西部竜峰山変成岩の層序，構造およびＫ‐Ａｒ年代"},{"@language":"ja","@value":"九州西部竜峰山変成岩の層序, 構造およびK-Ar年代"},{"@language":"ja-Kana","@value":"キュウシュウ セイブ リュウホウサン ヘンセイガン ノ ソウ ジョ コウゾウ オヨビ K-Ar ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206235159424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cathodoluminescence images of fault rocks found in the Suzuka granite, central Japan."},{"@value":"近畿地方鈴鹿花こう岩に認められる断層岩類のカソードルミネッセンス像"},{"@language":"ja","@value":"近畿地方鈴鹿花崗岩に認められる断層岩類のカソードルミネッセンス像"},{"@language":"ja-Kana","@value":"キンキ チホウ スズカ カコウガン ニ ミトメラレル ダンソウガンルイ ノ カ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237718400","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamic evolution of deformation microstructures in rocks. 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