{"@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/1363670319125042944.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2003gl019405"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2003GL019405"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003GL019405"}}],"dc:title":[{"@value":"Electrical resistivity structure at the SAFOD site from magnetotelluric exploration"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The magnetotelluric dataset collected on the San Andreas Fault at Parkfield has been re‐analyzed using superior inversion algorithms that have been developed in recent years. A combination of constrained inversion, forward modeling and synthetic inversion studies are used, and show that at the SAFOD site, the low resistivity fault zone extends to a depth of 2–3 km. An extended zone of low resistivity east of the San Andreas Fault may be connected to the SAF at seismogenic depths. The connection increases along the SAF to the northwest and may be related to the transition from locked to creeping seismic behavior.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319125042944","@type":"Researcher","foaf:name":[{"@value":"Martyn Unsworth"}],"jpcoar:affiliationName":[{"@value":"Institute for Geophysical Research, Department of Physics University of Alberta  Edmonton, Alberta Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319125042945","@type":"Researcher","foaf:name":[{"@value":"Paul A. Bedrosian"}],"jpcoar:affiliationName":[{"@value":"GeoForschungsZentrum  Potsdam Germany"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2004-05-18","prism:volume":"31","prism:number":"12","prism:startingPage":"L12S05"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2003GL019405"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2003GL019405"}],"createdAt":"2004-05-17","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567183382680448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid changes in the electrical state of the 1999 Izmit earthquake rupture zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230052352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Current Research Status and Future of Electromagnetic Survey Methods towards Integrated Analysis with Seismic Methods"},{"@language":"ja","@value":"電磁気法探査（ＥＭ法探査）技術の現状と展望―地震探査との統合型解析に向けて―"},{"@language":"ja-Kana","@value":"デンジキホウ タンサ EMホウ タンサ ギジュツ ノ ゲンジョウ ト テンボウ ジシン タンサ トノ トウゴウガタ カイセキ ニ ムケテ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942151033088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Imaging of a serpentinite complex in the Kamuikotan Zone, northern Japan, from magnetotelluric soundings"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942186660864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A 3-D electrical resistivity model beneath the focal zone of the 2008 Iwate-Miyagi Nairiku earthquake (M 7.2)"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892090759936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magnetotelluric transect of Unzen graben, Japan : conductors associated with normal faults"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2003gl019405"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1004-z_references_DOI_4tFsSHfcvWS3QfOzv0hIEozSPSE"},{"@type":"CROSSREF","@value":"10.5026/jgeography.117.997_references_DOI_MbA29PWcJskmO0FJNFA72bK5O6I"},{"@type":"CROSSREF","@value":"10.1038/ncomms3116_references_DOI_MbA29PWcJskmO0FJNFA72bK5O6I"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-50_references_DOI_MbA29PWcJskmO0FJNFA72bK5O6I"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01482-5_references_DOI_MbA29PWcJskmO0FJNFA72bK5O6I"}]}