{"@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/1360861704764292096.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/s41467-022-32923-8"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/s41467-022-32923-8.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/s41467-022-32923-8"}},{"identifier":{"@type":"PMID","@value":"36109510"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"In situ X-ray and acoustic observations of deep seismic faulting upon phase transitions in olivine"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n                  <jats:p>\n                    The activity of deep-focus earthquakes, which increases with depth from ~400 km to a peak at ~600 km, is enigmatic, because conventional brittle failure is unlikely to occur at elevated pressures. It becomes increasingly clear that pressure-induced phase transitions of olivine are responsible for the occurrence of the earthquakes, based on deformation experiments under pressure. However, many such experiments were made using analogue materials and those on mantle olivine are required to verify the hypotheses developed by these studies. Here we report the results of deformation experiments on (Mg,Fe)\n                    <jats:sub>2</jats:sub>\n                    SiO\n                    <jats:sub>4</jats:sub>\n                    olivine at 11−17 GPa and 860−1350 K, equivalent to the conditions of the slabs subducted into the mantle transition zone. We find that throughgoing faulting occurs only at very limited temperatures of 1100−1160 K, accompanied by intense acoustic emissions at the onset of rupture. Fault sliding aided by shear heating occurs along a weak layer, which is formed via linking-up of lenticular packets filled with nanocrystalline olivine and wadsleyite. Our study suggests that transformational faulting occurs on the isothermal surface of the metastable olivine wedge in slabs, leading to deep-focus earthquakes in limited regions and depth range.\n                  </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326211899392","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60570504"},{"@type":"NRID","@value":"1000060570504"},{"@type":"NRID","@value":"9000414373462"},{"@type":"NRID","@value":"9000004602744"},{"@type":"NRID","@value":"9000258744283"},{"@type":"NRID","@value":"9000391814678"},{"@type":"NRID","@value":"9000347191155"},{"@type":"NRID","@value":"9000283727688"},{"@type":"NRID","@value":"9000347192202"},{"@type":"NRID","@value":"9000283783639"},{"@type":"NRID","@value":"9000016936770"},{"@type":"NRID","@value":"9000396139379"},{"@type":"NRID","@value":"9000283729189"},{"@type":"NRID","@value":"9000347137929"},{"@type":"NRID","@value":"9000403551913"},{"@type":"NRID","@value":"9000283729168"},{"@type":"NRID","@value":"9000283729179"},{"@type":"NRID","@value":"9000347137969"},{"@type":"NRID","@value":"9000390426013"},{"@type":"NRID","@value":"9000347137996"},{"@type":"NRID","@value":"9000258434935"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000014904"}],"foaf:name":[{"@value":"Tomohiro Ohuchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861704764291979","@type":"Researcher","foaf:name":[{"@value":"Yuji Higo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861704764291855","@type":"Researcher","foaf:name":[{"@value":"Yoshinori Tange"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861704764292107","@type":"Researcher","foaf:name":[{"@value":"Takeshi Sakai"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861704764291983","@type":"Researcher","foaf:name":[{"@value":"Kohei Matsuda"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861704764292229","@type":"Researcher","foaf:name":[{"@value":"Tetsuo Irifune"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20411723"}],"prism:publicationName":[{"@value":"Nature Communications"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2022-09-15","prism:volume":"13","prism:number":"1"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://www.nature.com/articles/s41467-022-32923-8.pdf"},{"@id":"https://www.nature.com/articles/s41467-022-32923-8"}],"createdAt":"2022-09-15","modifiedAt":"2024-02-10","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Science","dc:title":"Science"},{"@id":"https://cir.nii.ac.jp/all?q=Q","dc:title":"Q"},{"@id":"https://cir.nii.ac.jp/all?q=Article","dc:title":"Article"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782013500160","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19H00722"},{"@type":"JGN","@value":"JP19H00722"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19H00722/"}],"notation":[{"@language":"ja","@value":"稍深発地震とスロースリップに対する超臨界水の効果：放射光その場観察実験による検証"},{"@language":"en","@value":"Role of aqueous fluid in occurrence of intraslab earthquakes"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050005508516260736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Poirierite, a dense metastable polymorph of magnesium iron silicate in shocked meteorites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135200384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Metastable olivine wedge and deep dry cold slab beneath southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135263744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High silicon self-diffusion coefficient in dry forsterite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425620224","@type":"Article","resourceType":"学術雑誌論文(journal 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