{"@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/1050282813184366848.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"HDL","@value":"http://hdl.handle.net/2433/234227"}},{"identifier":{"@type":"HDL","@value":"http://hdl.handle.net/10097/00130636"}},{"identifier":{"@type":"URI","@value":"https://tohoku.repo.nii.ac.jp/records/133246"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"11067477"}},{"identifier":{"@type":"DOI","@value":"10.1186/s40623-018-0788-6"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/digimeta/11067477"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/11067477"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/article/10.1186/s40623-018-0788-6/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/s40623-018-0788-6.pdf"}},{"identifier":{"@type":"HANDLE","@value":"2433/234227"}},{"identifier":{"@type":"NAID","@value":"120006517788"}},{"identifier":{"@type":"NAID","@value":"120006989892"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"Complex microseismic activity and depth-dependent stress field changes in Wakayama, southwestern Japan"}],"dc:language":"en","description":[{"type":"Abstract","notation":[{"@language":"en","@value":"We examined the spatial relationship between seismicity and upper crustal structure in the Wakayama region, northwestern Kii Peninsula, Japan, by investigating microearthquake focal mechanisms and the local stress field. The focal mechanisms of most events studied fall into three categories: (1) normal faulting with N–S-oriented T-axes mainly occurring at shallow depths, (2) reverse faulting with E–W-oriented P-axes dominating at intermediate depths, and (3) strike-slip faulting with N–S-oriented T-axes and E–W-oriented P-axes mainly seen at greater depths. The stress field varies with depth: the shallow part is characterized by a strike-slip-type stress regime with N–S tension and E–W compression, while the deep part is characterized by an E–W compressional stress regime consistent with reverse faulting. The depth-dependent stress regime can be explained by thermal stress caused by a heat source, as expected from geophysical observations. Geologic faults, acting as weak planes, might contribute to generate shallow normal fault-type and deeper strike-slip fault-type microearthquakes."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410003825208479488","@type":"Researcher","personIdentifier":[{"@type":"ORCID","@value":"0000-0002-7783-7242"},{"@type":"NRID","@value":"9000409996411"},{"@type":"NRID","@value":"9000410320350"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/maedasumire"}],"foaf:name":[{"@language":"en","@value":"Maeda, Sumire"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Graduate School of Science, Tohoku 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Toru"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Graduate School of Science, Tohoku 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Shinji"}],"jpcoar:affiliationName":[{"@language":"en","@value":"International Research Institute of Disaster Science, Tohoku University"}]},{"@id":"https://cir.nii.ac.jp/crid/1420845751148825856","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20743686"},{"@type":"NRID","@value":"1000020743686"},{"@type":"ORCID","@value":"0000-0002-1058-9811"},{"@type":"NRID","@value":"9000409849930"},{"@type":"NRID","@value":"9000409849926"},{"@type":"NRID","@value":"9000410320351"},{"@type":"NRID","@value":"9000406035253"},{"@type":"NRID","@value":"9000404481586"},{"@type":"NRID","@value":"9000414072569"},{"@type":"NRID","@value":"9000410320342"},{"@type":"NRID","@value":"9000405103758"},{"@type":"NRID","@value":"9000414241295"},{"@type":"NRID","@value":"9000398156125"},{"@type":"NRID","@value":"9000412000916"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/k-yoshida999"}],"foaf:name":[{"@language":"en","@value":"Yoshida, 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Hiroshi"},{"@language":"ja","@value":"片尾, 浩"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Research Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto University"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1892273591055297413","@type":"Researcher","foaf:name":[{"@value":"80221878"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658375583360","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80221878"},{"@type":"NRID","@value":"1000080221878"},{"@type":"ORCID","@value":"0000-0002-2070-6284"},{"@type":"NRID","@value":"9000364793842"},{"@type":"NRID","@value":"9000283242065"},{"@type":"NRID","@value":"9000001756558"},{"@type":"NRID","@value":"9000254263221"},{"@type":"NRID","@value":"9000254741761"},{"@type":"NRID","@value":"9000302392463"},{"@type":"NRID","@value":"9000397828942"},{"@type":"NRID","@value":"9000405118025"},{"@type":"NRID","@value":"9000000093580"},{"@type":"NRID","@value":"9000018699044"},{"@type":"NRID","@value":"9000014712485"},{"@type":"NRID","@value":"9000413694884"},{"@type":"NRID","@value":"9000405859175"},{"@type":"NRID","@value":"9000391405110"},{"@type":"NRID","@value":"9000254271068"},{"@type":"NRID","@value":"9000254741739"},{"@type":"NRID","@value":"9000252829743"},{"@type":"NRID","@value":"9000024111049"},{"@type":"NRID","@value":"9000398293225"},{"@type":"NRID","@value":"9000022222393"},{"@type":"NRID","@value":"9000329897343"},{"@type":"NRID","@value":"9000409470229"},{"@type":"NRID","@value":"9000000931349"},{"@type":"NRID","@value":"9000022220378"},{"@type":"NRID","@value":"9000254753870"},{"@type":"NRID","@value":"9000253256075"},{"@type":"NRID","@value":"9000403839320"},{"@type":"NRID","@value":"9000398156126"},{"@type":"NRID","@value":"9000386355295"},{"@type":"NRID","@value":"9000290824936"},{"@type":"NRID","@value":"9000001756744"},{"@type":"NRID","@value":"9000279888056"},{"@type":"NRID","@value":"9000408782886"},{"@type":"NRID","@value":"9000254263128"},{"@type":"NRID","@value":"9000364793808"},{"@type":"NRID","@value":"9000389566382"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/Manpuku-000"}],"foaf:name":[{"@value":"片尾, 浩"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18805981"},{"@type":"ISSN","@value":"13438832"},{"@type":"ISSN","@value":"18805981"},{"@type":"LISSN","@value":"13438832"}],"prism:publicationName":[{"@language":"en","@value":"Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Nature"}],"prism:publicationDate":"2018-02-07","prism:volume":"70","prism:startingPage":"21"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["© The Author(s) 2018. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made."],"url":[{"@id":"https://tohoku.repo.nii.ac.jp/records/133246"},{"@id":"http://id.ndl.go.jp/digimeta/11067477"},{"@id":"https://dl.ndl.go.jp/pid/11067477"},{"@id":"http://link.springer.com/article/10.1186/s40623-018-0788-6/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/s40623-018-0788-6.pdf"},{"@id":"http://hdl.handle.net/10097/00130636"},{"@id":"http://hdl.handle.net/2433/234227"}],"foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Microearthquake","dc:title":"Microearthquake"},{"@id":"https://cir.nii.ac.jp/all?q=Stress%20field","dc:title":"Stress field"},{"@id":"https://cir.nii.ac.jp/all?q=Heterogeneous%20structure","dc:title":"Heterogeneous structure"},{"@id":"https://cir.nii.ac.jp/all?q=Fluid","dc:title":"Fluid"},{"@id":"https://cir.nii.ac.jp/all?q=Heat%20source","dc:title":"Heat source"},{"@id":"https://cir.nii.ac.jp/all?q=Geological%20structure","dc:title":"Geological structure"}],"dcterms:subject":[{"subjectScheme":"Other","notation":[{"@language":"en","@value":"Microearthquake"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"Stress field"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"Heterogeneous structure"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"Fluid"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"Heat source"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"Geological structure"}]}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257255897216","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26109002"},{"@type":"JGN","@value":"JP26109002"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-26109002/"}],"notation":[{"@language":"ja","@value":"内陸地殻の強度と応力の解明"},{"@language":"en","@value":"Clarification of strength and stress of the inland crust"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285813661696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal dynamics: unified understanding of geodynamic processes at different time and length scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233288308864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stress before and after the 2011 great Tohoku‐oki earthquake and induced 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