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Power-laws between normal/shear stresses and steady-state wear rate, defined as (thickness of gouge formed)/(fault displacement), account for our data for diorite and granite at low velocities and most experimental data on wear of rocks reported in the literature. But an exponential law holds for wear of diorite at velocities greater than 0.11 m/s and its wear rate increases dramatically at seismic slip rates. A change from the power-law to the exponential law seems to be caused by frictional heating and thermal fracturing. Both power and exponential laws can describe data for granite. Sandstones exhibit complex wear behavior possibly due to development of shiny slickenside surface that suppresses wear. Our data for diorite indicate that, at the investigated normal stresses, only 0.004% of frictional work is consumed for gouge formation at velocities less than 0.11 m/s, but this fraction increases markedly with increasing velocity. Energy partition for gouge formation is not constant and changes with velocity during earthquakes."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848657255042818","@type":"Researcher","foaf:name":[{"@value":"Takehiro Hirose"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848657255042817","@type":"Researcher","foaf:name":[{"@value":"Kauzo Mizoguchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801183513216","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20112170"},{"@type":"NRID","@value":"1000020112170"},{"@type":"NRID","@value":"9000004606450"},{"@type":"NRID","@value":"9000020971621"},{"@type":"NRID","@value":"9000258413638"},{"@type":"NRID","@value":"9000254584616"},{"@type":"NRID","@value":"9000018323613"},{"@type":"NRID","@value":"9000347191148"},{"@type":"NRID","@value":"9000400192459"},{"@type":"NRID","@value":"9000351087674"},{"@type":"NRID","@value":"9000283906021"},{"@type":"NRID","@value":"9000258403580"},{"@type":"NRID","@value":"9000258412806"},{"@type":"NRID","@value":"9000017413618"},{"@type":"NRID","@value":"9000016929159"},{"@type":"NRID","@value":"9000283726456"},{"@type":"NRID","@value":"9000020956651"},{"@type":"NRID","@value":"9000258415734"},{"@type":"NRID","@value":"9000258413619"},{"@type":"NRID","@value":"9000258413648"},{"@type":"NRID","@value":"9000254584674"},{"@type":"NRID","@value":"9000020970828"},{"@type":"NRID","@value":"9000006041981"},{"@type":"NRID","@value":"9000258413636"},{"@type":"NRID","@value":"9000020115376"},{"@type":"NRID","@value":"9000020071310"},{"@type":"NRID","@value":"9000006083537"},{"@type":"NRID","@value":"9000006693707"},{"@type":"NRID","@value":"9000390925858"},{"@type":"NRID","@value":"9000020936698"},{"@type":"NRID","@value":"9000403550640"},{"@type":"NRID","@value":"9000005626842"},{"@type":"NRID","@value":"9000020071255"},{"@type":"NRID","@value":"9000350560226"},{"@type":"NRID","@value":"9000347082987"},{"@type":"NRID","@value":"9000253428433"},{"@type":"NRID","@value":"9000258412181"},{"@type":"NRID","@value":"9000258410570"},{"@type":"NRID","@value":"9000020963542"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0170880"}],"foaf:name":[{"@value":"Toshihiko Shimamoto"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01918141"}],"prism:publicationName":[{"@value":"Journal of Structural Geology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-05","prism:volume":"38","prism:startingPage":"102","prism:endingPage":"116"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0191814111002185?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0191814111002185?httpAccept=text/plain"}],"createdAt":"2011-12-23","modifiedAt":"2018-11-27","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782062633344","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21107004"},{"@type":"JGN","@value":"JP21107004"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21107004/"}],"notation":[{"@language":"ja","@value":"巨大地震断層の力学的・水理学的特性の解明"},{"@language":"en","@value":"Mechanical and hydrological properties of mega-earthquake thrusts"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782134141568","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22740334"},{"@type":"JGN","@value":"JP22740334"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22740334/"}],"notation":[{"@language":"ja","@value":"地震断層運動にともなう水素発生と地下生命圏のリンケージ"},{"@language":"en","@value":"Hydrogen generation by earthquake faulting and its implication for sub-surface biosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782149610112","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23340151"},{"@type":"JGN","@value":"JP23340151"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23340151/"}],"notation":[{"@language":"ja","@value":"高速域における断層強度の変位速度依存性および温度依存性の物質科学的解明"},{"@language":"en","@value":"Materials-science aspects on the velocity and temperature dependence of fault strength at high slip 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