{"@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/1363388846302863488.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1365-246x.1989.tb03357.x"}},{"identifier":{"@type":"URI","@value":"http://academic.oup.com/gji/article-pdf/98/2/343/1793811/98-2-343.pdf"}},{"identifier":{"@type":"NAID","@value":"30027003536"}}],"dc:title":[{"@value":"Water in the lower continental crust: modelling magnetotelluric and seismic reflection results"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1583668925863940992","@type":"Researcher","foaf:name":[{"@value":"R. D. Hyndman"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846302863488","@type":"Researcher","foaf:name":[{"@value":"P. M. Shearer"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0956540X"},{"@type":"EISSN","@value":"1365246X"}],"prism:publicationName":[{"@value":"Geophysical Journal International"}],"dc:publisher":[{"@value":"Oxford University Press (OUP)"}],"prism:publicationDate":"1989-08","prism:volume":"98","prism:number":"2","prism:startingPage":"343","prism:endingPage":"365"},"reviewed":"false","url":[{"@id":"http://academic.oup.com/gji/article-pdf/98/2/343/1793811/98-2-343.pdf"}],"createdAt":"2007-04-03","modifiedAt":"2019-03-24","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050573243559206016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimation of spatial distribution and fluid fraction of a potential supercritical geothermal reservoir by magnetotelluric data: a case study from Yuzawa geothermal field, NE Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981431089408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal magma pathway beneath Aso caldera inferred from three-dimensional electrical resistivity structure"},{"@value":"Crustal magma pathway beneath Aso caldera inferred from three‐dimensional electrical resistivity structure"},{"@value":"Crustal magma pathway beneath Aso caldera inferred from 3-D electrical resistivity structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214349850112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical image of subduction zone beneath northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229802607104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Triggering of earthquake swarms following the 2011 Tohoku megathrust earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229803726080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature and melt fraction distributions in a mantle wedge determined from the electrical conductivity structure: Application to one nonvolcanic and two volcanic regions in the Kyushu subduction zone, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708268763136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Electrical Resistivity Distribution Beneath the Beppu–Shimabara Graben With a Focus on Aso Caldera, Southwest Japan Subduction Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179755923584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐dimensional electromagnetic imaging of upwelling fluids in the Kyushu subduction zone, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088817024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of albite–(quartz)–water and albite–water–NaCl systems and its implication to the high conductivity anomalies in the continental crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182379010944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of fluid-bearing quartzite under lower crustal conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476823680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquake doublet in an active shear zone, southwest Japan: Constraints from geophysical and geochemical findings"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183245608320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Electrical Resistivity Modeling to Elucidate the Crustal Magma Supply System Beneath Aso Caldera, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186805154432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Localized extensional tectonics in an overall reverse-faulting regime, Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639279994496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of NaCl‐H<sub>2</sub>O fluid in the crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065343232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Unstable graphite films on grain boundaries in crustal rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065347584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of the serpentinised mantle and fluid flow in subduction zones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848661269048832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical Resistivity Structure and Helium Isotopes around Naruko Volcano, Northeastern Japan and Its Implication for the Distribution of Crustal Magma"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206509010944","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geomagnetic depth sounding in the Northern Apennines (Italy)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206509150208","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geoelectric structure beneath limestones of the Sao Francisco Basin, Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512534400","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Curie Point Depth variations to infer thermal structure of the crust at the African-Eurasian convergence zone, SW Turkey"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681485866752","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"2-D georesistivity structure in the central part of the northeastern Japan arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489290368","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rock microstructure in the deep extension of the Nagamachi-Rifu fault revealed by analysis of collocated seismic and magnetotelluric data"},{"@value":"Rock microstructure in the deep extension of the Nagamachi-Rifu fault revealed by analysis of collocated seismic and magnetotelluric data: Implication of strong deformation process"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490087168","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnetotelluric soundings across the Taubaté Basin, Southeast Brazil"},{"@value":"Magnetotelluric soundings across the Taubate Basin, Southeast Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490423424","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Origins of the lower crustal reflectivity in the Lützow-Holm Complex, Enderby Land, East Antarctica"},{"@value":"Origins of the lower crustal reflectivity in the Lutzow-Holm Complex, Enderby Land, East Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1523669554818972032","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"Rock microstructure in the deep extension of the Nagamachi-Rifu fault revealed by analysis of collocated seismic and magnetotelluric data: Implication of strong deformation process"},{"@language":"ja-Kana","@value":"Rock microstructure in the deep extension of the Nagamachi Rifu fault revealed by analysis of collocated seismic and magnetotelluric data Implication of strong deformation process"}]},{"@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"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046916224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of brine-bearing quartzite at 1 GPa : implications for fluid content and salinity of the crust"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.1989.tb03357.x"},{"@type":"CIA","@value":"30027003536"},{"@type":"CROSSREF","@value":"10.1002/2015jb012028_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1002/2014jb011598_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1002/2015gl063308_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-2_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1004-z_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/bf03351578_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/bf03352395_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/bf03353399_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1029/2018jb015506_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.05.013_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/bf03351821_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/bf03353050_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1002/2014jb011336_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1029/2018jb015951_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/s40562-015-0030-3_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1029/2021jb022911_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1002/2015jb012219_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/bf03351577_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1186/bf03353361_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1002/2016gl070315_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1155/2010/738139_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2011.04.003_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2012.03.007_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.12.021_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2014.07.025_references_DOI_IEkejRr0OF5VOSWTcJ5RpRSb3dD"}]}