{"@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/1390001206513367296.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03351777"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"6686699"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/6686699"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I6686699"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/8842301"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03351777.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03351777/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03351777"}},{"identifier":{"@type":"NAID","@value":"10011769305"}},{"identifier":{"@type":"NAID","@value":"130003956346"}}],"dc:title":[{"@language":"en","@value":"Resistivity structure in the western part of the fault rupture zone associated with the 1999 Izmit earthquake and its seismogenic implication"},{"@value":"Resistivity structure in the western part of the fault repture zone associated with the 1999 Izmit earthquake and its seismogenic implication"},{"@value":"Resistivity structure in the western part of the fault rupture zone associated with the 1999 İzmit earthquake and its seismogenic implication"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Magnetotelluric (MT) surveys were carried out along some profiles crossing the fault rupture zone associated with the Izmit earthquake which took place on 17 August 1999 in the western part of the North Anatolian Fault Zone (NAFZ). In this paper, we focus on the western part of the fault rupture zone where two different groups of seismicity followed the Izmit earthquake. One group was seen along a narrow belt and corresponds to aftershocks occurring along the fault rupture zone. The other was seen in a circular region and represents a swarm activity, presumably triggered by the occurrence of the Izmit earthquake. Two-dimensional inversion was performed for the MT data acquired along two profiles; one crosses the western end of the fault rupture zone and the other is located in the west of the swarm activity area. In the former case, aftershocks tended to occur in a resistive zone underlain by a moderately conductive zone, as was the case for the hypocenter area. In the latter case, the swarm activity tends to be confined in a conductive zone below a highly resistive zone. This activity is likely to be triggered through pore-pressure changes associated with the Izmit earthquake."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410001206509226114","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254262001"},{"@type":"NRID","@value":"9000000237214"}],"foaf:name":[{"@language":"en","@value":"Tank S. B."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Planetary Sciences, Tokyo Institute of Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001206513367301","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Honkura Y."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Planetary Sciences, Tokyo Institute of Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001206513367296","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000001098981"}],"foaf:name":[{"@language":"en","@value":"Ogawa Y."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Volcanic Fluid Research Center, Tokyo Institute of Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001206513367296","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000001098981"}],"foaf:name":[{"@language":"en","@value":"Oshiman N."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Disaster Prevention Research Institute, Kyoto University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001206513367299","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Tuncçer M. K."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Kandilli Observatory and Earthquake Research Institute, Bogazicçi University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001206513367303","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Matsushima M."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Earth and Planetary Sciences, Tokyo Institute of Technology"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001206509226117","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000254262000"},{"@type":"NRID","@value":"9000000237215"}],"foaf:name":[{"@language":"en","@value":"Çelik C."}],"jpcoar:affiliationName":[{"@language":"en","@value":"Kandilli Observatory and Earthquake Research Institute, Bogazicçi University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001206513367300","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Isikara M."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13438832"},{"@type":"EISSN","@value":"18805981"},{"@type":"NDL_BIB_ID","@value":"000000159136"},{"@type":"ISSN","@value":"13438832"},{"@type":"LISSN","@value":"13438832"},{"@type":"NCID","@value":"AA11211921"}],"prism:publicationName":[{"@language":"en","@value":"Earth, Planets and Space"},{"@language":"ja","@value":"Ｅａｒｔｈ，　Ｐｌａｎｅｔｓ　ａｎｄ　Ｓｐａｃｅ"},{"@language":"en","@value":"Earth Planets Space"},{"@language":"ja","@value":"Ｅａｒｔｈ　Ｐｌａｎｅｔｓ　Ｓｐａｃｅ"}],"dc:publisher":[{"@language":"en","@value":"Society of Geomagnetism and Earth, Planetary and Space Sciences, The Seismological Society of Japan, The Volcanological Society of Japan , The Geodetic Society of Japan , The Japanese Society for Planetary Sciences"},{"@language":"ja","@value":"地球電磁気・地球惑星圏学会 、公益社団法人 日本地震学会、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会"}],"prism:publicationDate":"2003","prism:volume":"55","prism:number":"7","prism:startingPage":"437","prism:endingPage":"442"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/6686699"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I6686699"},{"@id":"https://dl.ndl.go.jp/pid/8842301"},{"@id":"https://link.springer.com/content/pdf/10.1186/BF03351777.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03351777/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03351777"}],"availableAt":"2003","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Magnetotellurics","dc:title":"Magnetotellurics"},{"@id":"https://cir.nii.ac.jp/all?q=resistivity%20structure","dc:title":"resistivity structure"},{"@id":"https://cir.nii.ac.jp/all?q=Izmit%20earthquake","dc:title":"Izmit earthquake"},{"@id":"https://cir.nii.ac.jp/all?q=North%20Anatolian%20Fault%20Zone","dc:title":"North Anatolian Fault Zone"},{"@id":"https://cir.nii.ac.jp/all?q=seismogenic%20zone","dc:title":"seismogenic zone"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050587981430736000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismicity controlled by resistivity structure : the 2016 Kumamoto earthquakes, Kyushu Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002217556297344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical characterization of the North Anatolian Fault Zone underneath the Marmara Sea, Turkey by ocean bottom magnetotellurics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011143760339968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional magnetotelluric modeling using difference equations; theory and comparisons to integral 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NE Japan Back Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419672695936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tomography of the Source Area of the 1995 Kobe Earthquake: Evidence for Fluids at the Hypocenter?"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420276044288","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Electromagnetic heterogeneity of the seismogenic region of 1962 M6.5 Northern Miyagi Earthquake, northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421060973568","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Conductive crust imaged in western Turkey by MT"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893997333248","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Aftershock Activity of the 1999 Izmit, Turkey, Earthquake Revealed from Microearthquake 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V<SUB>p</SUB>, V<SUB>s</SUB> and V<SUB>p</SUB>/V<SUB>s</SUB> in the upper crust of the Marmara region, NW Turkey"},{"@value":"Three-dimensional structure of Vp, Vs and Vp/Vs in the upper crust of the Marmara region, NW Turkey"},{"@value":"The three-dimensional structure of Vp, Vs and Vp/Vs in the upper crust of the Marmara region, NW Turkey"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511645312","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Resistivity structure around the hypocentral area of the 1984 Western Nagano Prefecture earthquake in central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512576512","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mid-crustal electrical conductors and their correlations to seismicity and deformation at Itoigawa-Shizuoka Tectonic Line, Central Japan"},{"@value":"Mid-crustal conductors and their correlations to the seismicity and deformation at Itoigawa–Shizuoka tectonic line, Central Japan"},{"@value":"Mid-crustal electrical conductors and their correlations to seismicity and deformation at Itoigawa-Shizuoka Tectonic Line"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512786688","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lateral inhomogeneity deduced from 3-D magnetotelluric modeling around the hypocentral area of the 1984Western Nagano Prefecture earthquake, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206514108672","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"On the geoelectric structure of major strike-slip faults and shear zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489951232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Resistivity structure across Itoigawa-Shizuoka 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