{"@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/1363670320100119808.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2006jb004738"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2006JB004738"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2006JB004738"}}],"dc:title":[{"@value":"Nondestructive continuous physical property measurements of core samples recovered from hole B, Taiwan Chelungpu‐Fault Drilling Project"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The Taiwan Chelungpu‐Fault Drilling Project was undertaken in 2002 to investigate the faulting mechanism of the 1999 <jats:italic>M</jats:italic><jats:sub>w</jats:sub> 7.6 Taiwan Chi‐Chi earthquake. Hole B penetrated the Chelungpu fault, and core samples were recovered from between 948.42‐ and 1352.60‐m depth. Three major zones, designated FZB1136 (fault zone at 1136‐m depth in hole B), FZB1194, and FZB1243, were recognized in the core samples as active fault zones within the Chelungpu fault. Nondestructive continuous physical property measurements, conducted on all core samples, revealed that the three major fault zones were characterized by low gamma ray attenuation (GRA) densities and high magnetic susceptibilities. Extensive fracturing and cracks within the fault zones and/or loss of atoms with high atomic number, but not a measurement artifact, might have caused the low GRA densities, whereas the high magnetic susceptibility values might have resulted from the formation of magnetic minerals from paramagnetic minerals by frictional heating. Minor fault zones were characterized by low GRA densities and no change in magnetic susceptibility, and the latter may indicate that these minor zones experienced relatively low frictional heating. Magnetic susceptibility in a fault zone may be key to the determination that frictional heating occurred during an earthquake on the fault.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320100119812","@type":"Researcher","foaf:name":[{"@value":"Tetsuro Hirono"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Space Science, Graduate School of Science Osaka University  Toyonaka, Osaka Japan"},{"@value":"Kochi Institute for Core Sample Research Japan Agency for Marine‐Earth Science and Technology  Nankoku, Kochi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016870359379200","@type":"Researcher","foaf:name":[{"@value":"En‐Chao Yeh"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences National Taiwan University  Taipei Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119815","@type":"Researcher","foaf:name":[{"@value":"Weiren Lin"}],"jpcoar:affiliationName":[{"@value":"Kochi Institute for Core Sample Research Japan Agency for Marine‐Earth Science and Technology  Nankoku, Kochi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119819","@type":"Researcher","foaf:name":[{"@value":"Hiroki Sone"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics, School of Earth Sciences Stanford University  Stanford California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119816","@type":"Researcher","foaf:name":[{"@value":"Toshiaki Mishima"}],"jpcoar:affiliationName":[{"@value":"Center for Advanced Marine Core Research Kochi University  Nankoku, Kochi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119683","@type":"Researcher","foaf:name":[{"@value":"Wonn Soh"}],"jpcoar:affiliationName":[{"@value":"Kochi Institute for Core Sample Research Japan Agency for Marine‐Earth Science and Technology  Nankoku, Kochi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119808","@type":"Researcher","foaf:name":[{"@value":"Yoshitaka Hashimoto"}],"jpcoar:affiliationName":[{"@value":"Department of Natural Environmental Science, Faculty of Science Kochi University  Kochi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119687","@type":"Researcher","foaf:name":[{"@value":"Osamu Matsubayashi"}],"jpcoar:affiliationName":[{"@value":"Institute for Geo‐Resources and Environment National Institute of Advanced Industrial Science and Technology  Tsukuba Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119684","@type":"Researcher","foaf:name":[{"@value":"Kan Aoike"}],"jpcoar:affiliationName":[{"@value":"Center for Deep Earth Exploration Japan Agency for Marine‐Earth Science and Technology  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119688","@type":"Researcher","foaf:name":[{"@value":"Hisao Ito"}],"jpcoar:affiliationName":[{"@value":"Center for Deep Earth Exploration Japan Agency for Marine‐Earth Science and Technology  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119822","@type":"Researcher","foaf:name":[{"@value":"Masataka Kinoshita"}],"jpcoar:affiliationName":[{"@value":"Institute for Research on Earth Evolution Japan Agency for Marine‐Earth Science and Technology  Yokosuka Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119686","@type":"Researcher","foaf:name":[{"@value":"Masafumi Murayama"}],"jpcoar:affiliationName":[{"@value":"Center for Advanced Marine Core Research Kochi University  Nankoku, Kochi Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016870359379201","@type":"Researcher","foaf:name":[{"@value":"Sheng‐Rong Song"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences National Taiwan University  Taipei Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016870359379203","@type":"Researcher","foaf:name":[{"@value":"Kuo‐Fong Ma"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics National Central University  Jhongli Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016870359379328","@type":"Researcher","foaf:name":[{"@value":"Jih‐Hao Hung"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics National Central University  Jhongli Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016870359379202","@type":"Researcher","foaf:name":[{"@value":"Chien‐Ying Wang"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics National Central University  Jhongli Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380016870359379204","@type":"Researcher","foaf:name":[{"@value":"Yi‐Ben Tsai"}],"jpcoar:affiliationName":[{"@value":"Institute of Geophysics National Central University  Jhongli Taiwan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119820","@type":"Researcher","foaf:name":[{"@value":"Tomomi Kondo"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119817","@type":"Researcher","foaf:name":[{"@value":"Masahiro Nishimura"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119811","@type":"Researcher","foaf:name":[{"@value":"Soichi Moriya"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119813","@type":"Researcher","foaf:name":[{"@value":"Tomoyuki Tanaka"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119689","@type":"Researcher","foaf:name":[{"@value":"Toru Fujiki"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119690","@type":"Researcher","foaf:name":[{"@value":"Lena Maeda"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119818","@type":"Researcher","foaf:name":[{"@value":"Hiroaki Muraki"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119680","@type":"Researcher","foaf:name":[{"@value":"Toshikatsu Kuramoto"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119682","@type":"Researcher","foaf:name":[{"@value":"Kazuhiro Sugiyama"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320100119809","@type":"Researcher","foaf:name":[{"@value":"Toshikatsu Sugawara"}],"jpcoar:affiliationName":[{"@value":"Marine Works Japan Ltd.  Yokohama Japan"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1894242817750617863","@type":"Researcher","foaf:name":[{"@value":"0 Pre-GFZ, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2007-07","prism:volume":"112","prism:number":"B7","prism:startingPage":"B07404"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2006JB004738"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2006JB004738"}],"createdAt":"2007-07-06","modifiedAt":"2023-10-12","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550%20-%20Earth%20sciences","dc:title":"550 - Earth sciences"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050866514666885120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Investigation of the records of earthquake slip in carbonaceous materials from the Taiwan Chelungpu fault by means of infrared and Raman spectroscopies"},{"@value":"Investigation of the records of earthquake slip in carbonaceous materials from the <scp>T</scp>aiwan <scp>C</scp>helungpu fault by means of infrared and <scp>R</scp>aman spectroscopies"}]},{"@id":"https://cir.nii.ac.jp/crid/1050866514666966656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of slip parameters associated with frictional heating during the 1999 Taiwan Chi-Chi earthquake by vitrinite reflectance geothermometry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216175278336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Localized rotation of principal stress around faults and fractures determined from borehole breakouts in hole B of the Taiwan Chelungpu-fault Drilling Project (TCDP)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183492239872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Preservation of amorphous ultrafine material: A proposed proxy for slip during recent earthquakes on active faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453588608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Blackening of fault gouge by comminution and pyrolysis of carbonaceous materials during earthquake slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680294989312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"台湾チェルンプ断層掘削における成果"},{"@language":"en","@value":"Scientific Result of material analyses of the Taiwan Chelungpu fault Drilling Project (TCDP)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680294998912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Porosity profile within the Taiwan Chelungpu Fault, reconstructed from X-ray computed tomography images"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213889280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Overview of scientific results of the deep drilling project of the Chelungpu Fault, upon which the 1999 Chi-Chi (Taiwan) earthquake occurred: Main findings and future research"},{"@language":"ja","@value":"1999年台湾集集地震を引き起こしたチェルンプ断層の深部掘削の成果概要－明らかになってきた断層岩の物質科学と今後の課題－"},{"@language":"ja-Kana","@value":"1999ネン タイワンシュウシュウ ジシン オ ヒキオコシタ チェルンプ ダンソウ ノ シンブ クッサク ノ セイカ ガイヨウ アキラカ ニ ナッテ キタ ダンソウガン ノ ブッシツ カガク ト コンゴ ノ カダイ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2006jb004738"},{"@type":"OPENAIRE","@value":"doi_dedup___::87836f6c8c79b7db663103b90272d586"},{"@type":"CROSSREF","@value":"10.1002/2014gc005622_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-28_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"},{"@type":"CROSSREF","@value":"10.1038/srep36536_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.9.2_15_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"},{"@type":"CROSSREF","@value":"10.5575/geosoc.115.488_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.03.039_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"},{"@type":"CROSSREF","@value":"10.5918/jamstecr.9.2_95_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2009.06.020_references_DOI_9WEDtk95CISQe93ZrWFbiqx0JoZ"}]}