One important factor controlling crustal strength is fault zone development. A fault can mature through multiple stages where small faults are generated by rupturing homogeneous media, and are partially connected each other, with large deformations locally concentrated along a major fault. Fault geometry, stress field, and seismic activity, which are detectable with seismic observations, may depend on the stage of fault evolution. At the same time, fault distribution and slip properties observed in a geological survey also provide important information on constraints to fault development. In particular, comparing fault distribution and direction between seismological analyses and geological observations plays an important role in understanding the history of fault zone evolution. A bottleneck in the seismological approach to investigating fault zone development is low spatial resolution due to low spatial density and number of seismic stations. A key element for understanding fault zone development in the crust based on seismic observations is discussed. “0.1 manten” hyper dense seismic observations carried out in the focal area of the 2000 Western Tottori earthquake (M 7.3) are introduced along with the preliminary results of a data analysis.
"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801209043968","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50159547"},{"@type":"NRID","@value":"1000050159547"},{"@type":"ORCID","@value":"0000-0003-0808-0757"},{"@type":"CINII_AUTHOR_ID","@value":"DA19070894"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA19070894#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA19070894"},{"@type":"NRID","@value":"9000391400827"},{"@type":"NRID","@value":"9000007771930"},{"@type":"NRID","@value":"9000266443229"},{"@type":"NRID","@value":"9000001755585"},{"@type":"NRID","@value":"9000237727344"},{"@type":"NRID","@value":"9000391406325"},{"@type":"NRID","@value":"9000254262874"},{"@type":"NRID","@value":"9000254262262"},{"@type":"NRID","@value":"9000254262275"},{"@type":"NRID","@value":"9000254741787"},{"@type":"NRID","@value":"9000405103777"},{"@type":"NRID","@value":"9000405521311"},{"@type":"NRID","@value":"9000014140037"},{"@type":"NRID","@value":"9000016835652"},{"@type":"NRID","@value":"9000024133117"},{"@type":"NRID","@value":"9000254270909"},{"@type":"NRID","@value":"9000254262395"},{"@type":"NRID","@value":"9000411621709"},{"@type":"NRID","@value":"9000000931512"},{"@type":"NRID","@value":"9000023738402"},{"@type":"NRID","@value":"9000413694875"},{"@type":"NRID","@value":"9000397969348"},{"@type":"NRID","@value":"9000408484410"},{"@type":"NRID","@value":"9000404679282"},{"@type":"NRID","@value":"9000254741736"},{"@type":"NRID","@value":"9000009700397"},{"@type":"NRID","@value":"9000019055012"},{"@type":"NRID","@value":"9000023769998"},{"@type":"NRID","@value":"9000406034850"},{"@type":"NRID","@value":"9000254754012"},{"@type":"NRID","@value":"9000254263027"},{"@type":"NRID","@value":"9000000931355"},{"@type":"NRID","@value":"9000398128080"},{"@type":"NRID","@value":"9000370763591"},{"@type":"NRID","@value":"9000391401467"},{"@type":"NRID","@value":"9000254741488"},{"@type":"NRID","@value":"9000399763390"},{"@type":"NRID","@value":"9000241836780"},{"@type":"NRID","@value":"9000023757795"},{"@type":"NRID","@value":"9000329897341"},{"@type":"NRID","@value":"9000409470212"},{"@type":"NRID","@value":"9000409470230"},{"@type":"NRID","@value":"9000254262312"},{"@type":"NRID","@value":"9000410320304"},{"@type":"NRID","@value":"9000241208979"},{"@type":"NRID","@value":"9000256898259"},{"@type":"NRID","@value":"9000023730730"},{"@type":"NRID","@value":"9000397969380"},{"@type":"NRID","@value":"9000391404680"},{"@type":"NRID","@value":"9000391403675"},{"@type":"NRID","@value":"9000254754141"},{"@type":"NRID","@value":"9000254262388"},{"@type":"NRID","@value":"9000254753991"},{"@type":"NRID","@value":"9000016787972"},{"@type":"NRID","@value":"9000000767630"},{"@type":"NRID","@value":"9000000931412"},{"@type":"NRID","@value":"9000391406207"},{"@type":"NRID","@value":"9000000093589"},{"@type":"NRID","@value":"9000254262910"},{"@type":"NRID","@value":"9000254262865"},{"@type":"NRID","@value":"9000254741449"},{"@type":"NRID","@value":"9000279888051"},{"@type":"NRID","@value":"9000382633918"},{"@type":"NRID","@value":"9000408575960"},{"@type":"NRID","@value":"9000412040960"},{"@type":"NRID","@value":"9000376548183"},{"@type":"NRID","@value":"9000000767610"},{"@type":"NRID","@value":"9000000931373"},{"@type":"NRID","@value":"9000254263125"},{"@type":"NRID","@value":"9000344119288"},{"@type":"NRID","@value":"9000256898265"},{"@type":"NRID","@value":"9000023944794"},{"@type":"NRID","@value":"9000409996417"},{"@type":"NRID","@value":"9000375914881"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/iio"}],"foaf:name":[{"@language":"en","@value":"IIO Yoshihisa"},{"@language":"ja","@value":"飯尾 能久"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"京都大学防災研究所"},{"@language":"en","@value":"Disaster Prevention Research Institute, Kyoto University"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801206085504","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20359201"},{"@type":"NRID","@value":"1000020359201"},{"@type":"ORCID","@value":"0000-0002-2645-3441"},{"@type":"NRID","@value":"9000006033705"},{"@type":"NRID","@value":"9000254262892"},{"@type":"NRID","@value":"9000403164073"},{"@type":"NRID","@value":"9000258283123"},{"@type":"NRID","@value":"9000413694885"},{"@type":"NRID","@value":"9000345423093"},{"@type":"NRID","@value":"9000019055006"},{"@type":"NRID","@value":"9000410949145"},{"@type":"NRID","@value":"9000283310701"},{"@type":"NRID","@value":"9000390916926"},{"@type":"NRID","@value":"9000410320306"},{"@type":"NRID","@value":"9000318561437"},{"@type":"NRID","@value":"9000265260296"},{"@type":"NRID","@value":"9000367411282"},{"@type":"NRID","@value":"9000254741492"},{"@type":"NRID","@value":"9000403164400"},{"@type":"NRID","@value":"9000279888019"},{"@type":"NRID","@value":"9000014234698"},{"@type":"NRID","@value":"9000025069143"},{"@type":"NRID","@value":"9000323844364"},{"@type":"NRID","@value":"9000356478482"},{"@type":"NRID","@value":"9000408484442"},{"@type":"NRID","@value":"9000288834599"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/aitarokato"}],"foaf:name":[{"@language":"en","@value":"KATO Aitaro"},{"@language":"ja","@value":"加藤 愛太郎"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Earthquake Research Institute, University of Tokyo"},{"@language":"ja","@value":"東京大学地震研究所"}]},{"@id":"https://cir.nii.ac.jp/crid/1410004222631011075","@type":"Researcher","personIdentifier":[{"@type":"ORCID","@value":"0000-0002-6893-1309"},{"@type":"NRID","@value":"9000410320305"}],"foaf:name":[{"@language":"en","@value":"SAKAI Shinichi"},{"@language":"ja","@value":"酒井 慎一"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Earthquake Research Institute, University of Tokyo"},{"@language":"ja","@value":"東京大学地震研究所"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001204305605632","@type":"Researcher","personIdentifier":[{"@type":"ORCID","@value":"0000-0001-7925-801X"},{"@type":"NRID","@value":"9000000465428"},{"@type":"NRID","@value":"9000283242075"},{"@type":"NRID","@value":"9000001756385"},{"@type":"NRID","@value":"9000370253957"},{"@type":"NRID","@value":"9000254741763"},{"@type":"NRID","@value":"9000410949905"},{"@type":"NRID","@value":"9000261679983"},{"@type":"NRID","@value":"9000391406618"},{"@type":"NRID","@value":"9000391405629"},{"@type":"NRID","@value":"9000254741711"},{"@type":"NRID","@value":"9000254741745"},{"@type":"NRID","@value":"9000391404243"},{"@type":"NRID","@value":"9000254741487"},{"@type":"NRID","@value":"9000409470222"},{"@type":"NRID","@value":"9000410320303"},{"@type":"NRID","@value":"9000391405894"},{"@type":"NRID","@value":"9000254271183"},{"@type":"NRID","@value":"9000254741448"},{"@type":"NRID","@value":"9000410320270"},{"@type":"NRID","@value":"9000279888061"},{"@type":"NRID","@value":"9000254741706"},{"@type":"NRID","@value":"9000391406500"},{"@type":"NRID","@value":"9000391405548"},{"@type":"NRID","@value":"9000254263127"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/sevo_matu"}],"foaf:name":[{"@language":"en","@value":"MATSUMOTO Satoshi"},{"@language":"ja","@value":"松本 聡"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Faculty of Science, Kyushu University"},{"@language":"ja","@value":"九州大学大学院理学研究院"}]},{"@id":"https://cir.nii.ac.jp/crid/1410004222631011076","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000410320307"}],"foaf:name":[{"@language":"en","@value":"Group for “0.1 Manten” Hyper Dense Seismic Observation"},{"@language":"ja","@value":"0.1満点地震観測グループ"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"九州大学大学院理学研究院・理学府：松本 聡，松島 健，志藤あずさ，千葉慶太，手操佳子（現：気象庁），神薗めぐみ，光岡郁穂，村松 弾，岩佐優一，武石貢佑（現：気象庁），林田祐人，湯浅雄平；京都大学防災研究所：飯尾能久，冨坂和秀，米田 格，澤田麻沙代，長岡愛理，波岸彩子，中川 潤，三浦 勉，津田寛大，加藤慎也，伊藤喜宏；東京大学地震研究所：酒井慎一，加藤愛太郎，岩崎貴哉，池澤賢志，大塚宏徳，佐伯綾香，諏訪祥士（現：気象庁），芹澤正人，西本太郎，藤田親亮，増田正孝，森 健彦（現：気象庁）；関西大学社会安全学部：林 能成；高知大学高知地震観測所：大久保慎人・山品匡史；鳥取大学工学研究科：香川敬生・野口竜也；島根大学総合理工学部：向吉秀樹・内田嗣人・大久雅貴・奥田悠大・高松洋太・長畑友貴・橋本 匡・松原 透"},{"@language":"en","@value":"Matsumoto, S., Matsushima, T., Shito, A., Chiba, K., Teguri, K., Kamizono, M., Mitsuoka, A., Muramatsu, D., Iwasa, Y., Takeishi, K., Hayashida, Y., Yuasa, Y., Iio, Y., Tomisaka, K., Yoneda, I., Sawada, M., Nagaoka, A., Namigisi, A., Nakagawa, J., Miura, T.,Tsuda, H., Katoh, S., Ito, Y., Sakai, S., Kato, A., Iwasaki, T., Ikezawa, K., Otsuka, H., Saeki, A., Suwa, S., Serizawa, M., Nishimoto, T., Fujita, C., Masuda, M., Mori, T., Hayashi, Y., Okubo, M., Yamashina, T., Kagawa, T., Noguchi, T., Mokoyoshi, H., Uchida, H., Okuda, Y., Takamatsu, Y., Nagahata, Y., Hashimoto, T. and Matsubara, T."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0022135X"},{"@type":"LISSN","@value":"0022135X"},{"@type":"EISSN","@value":"18840884"},{"@type":"NDL_BIB_ID","@value":"000000014613"},{"@type":"ISSN","@value":"0022135X"},{"@type":"NCID","@value":"AN00322536"}],"prism:publicationName":[{"@language":"en","@value":"Journal of Geography (Chigaku Zasshi)"},{"@language":"ja","@value":"地学雑誌"},{"@language":"ja","@value":"地學雜誌"},{"@language":"en","@value":"J. Geogr."},{"@language":"en","@value":"Jour. Geogr."},{"@language":"en","@value":"Journal of Geography"},{"@language":"ja","@value":"地学雑"},{"@language":"en","@value":"Journal of Geography (Chigaku Zasshi)"},{"@language":"en","@value":"Journal of Geography(Chigaku Zasshi)"},{"@language":"ja","@value":"地學雜誌"}],"dc:publisher":[{"@language":"en","@value":"Tokyo Geographical Society"},{"@language":"ja","@value":"公益社団法人 東京地学協会"}],"prism:publicationDate":"2020-08-25","prism:volume":"129","prism:number":"4","prism:startingPage":"511","prism:endingPage":"527"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/030621757"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I030621757"},{"@id":"https://www.jstage.jst.go.jp/article/jgeography/129/4/129_129.511/_pdf"}],"availableAt":"2020-08-25","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=fault%20development","dc:title":"fault development"},{"@id":"https://cir.nii.ac.jp/all?q=seismic%20observation","dc:title":"seismic observation"},{"@id":"https://cir.nii.ac.jp/all?q=0.1%20manten%20hyper%20dense%20seismic%20observation","dc:title":"0.1 manten hyper dense seismic observation"},{"@id":"https://cir.nii.ac.jp/all?q=2000%20Western%20Tottori%20earthquake","dc:title":"2000 Western Tottori earthquake"},{"@id":"https://cir.nii.ac.jp/all?q=stress%20field","dc:title":"stress field"},{"@id":"https://cir.nii.ac.jp/all?q=%E6%96%AD%E5%B1%A4%E5%B8%AF%E7%99%BA%E9%81%94%E9%81%8E%E7%A8%8B","dc:title":"断層帯発達過程"},{"@id":"https://cir.nii.ac.jp/all?q=%E7%A8%A0%E5%AF%86%E5%9C%B0%E9%9C%87%E8%A6%B3%E6%B8%AC","dc:title":"稠密地震観測"},{"@id":"https://cir.nii.ac.jp/all?q=0.1%E6%BA%80%E7%82%B9%E5%9C%B0%E9%9C%87%E8%A6%B3%E6%B8%AC","dc:title":"0.1満点地震観測"},{"@id":"https://cir.nii.ac.jp/all?q=2000%E5%B9%B4%E9%B3%A5%E5%8F%96%E7%9C%8C%E8%A5%BF%E9%83%A8%E5%9C%B0%E9%9C%87","dc:title":"2000年鳥取県西部地震"},{"@id":"https://cir.nii.ac.jp/all?q=%E5%BF%9C%E5%8A%9B%E5%A0%B4","dc:title":"応力場"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282256992236928","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19H05449"},{"@type":"JGN","@value":"JP19H05449"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-WRAPUP-19H05449/"}],"notation":[{"@language":"ja","@value":"地殻ダイナミクス －東北沖地震後の内陸変動の統一的理解－"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202707280384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001335851923328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Why do aftershocks occur? Relationship between mainshock rupture and aftershock sequence based on highly resolved hypocenter and focal mechanism distributions"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022996649445760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Prestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (M7.3)"},{"@value":"Prestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (M7.3)"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564285791632128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564288453609216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Hypocenter Migration and Seismicity Pattern Change in the Yamagata-Fukushima Border, NE Japan, Caused by Fluid Movement and Pore Pressure Variation"}]},{"@id":"https://cir.nii.ac.jp/crid/1050867421579577216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inelastic strain in the hypocentral region of the 2000 Western Tottori earthquake (M 7.3) inferred from aftershock seismic moment tensors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229807889536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seismic velocity structure in the source region of the 2016 Kumamoto earthquake sequence, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230122138880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Imaging the source regions of normal faulting sequences induced by the 2011 M9.0 Tohoku‐Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704779197696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Changes in the stress field after the 2008 M7.2 Iwate‐Miyagi Nairiku earthquake in northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500126336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Determining changes in the state of stress associated with an earthquake via combined focal mechanism and moment tensor analysis: Application to the 2013 Awaji Island earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621436583552","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Estimation of the stress field in the region of the 2000 Western Tottori Earthquake: Using numerous aftershock focal mechanisms"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905159579520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Minna de Honkoku: Citizen-Participation Transcription Project for Japanese Historical Documents"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568468126498176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Non‐Double‐Couple Microearthquakes in the Focal Area of the 2000 Western Tottori Earthquake (M 7.3) via Hyperdense Seismic Observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570878253952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Strength of the lithosphere: Constraints imposed by laboratory experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044986287488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Imaging the seismic structure and stress field in the source region of the 2004 mid‐Niigata prefecture earthquake: Structural zones of weakness and seismogenic stress concentration by ductile flow"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519529699840","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional velocity structure in the source region of the Noto Hanto Earthquake in 2007 imaged by a dense seismic observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520145153280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Slip on 'weak' faults by the rotation of regional stress in the fracture damage zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995338990720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Orientation of the stress field surrounding the creeping section of the San Andreas Fault: Evidence for a narrow mechanically weak fault zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945516317312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Temporal Stress Changes Caused by Earthquakes: A Review"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895730220160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stress before and after the 2002 Denali fault earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896334857472","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Imaging the heterogeneous source area of the 2003 M6.4 northern Miyagi earthquake, NE Japan, by double-difference tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368511029888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Imaging the source area of the 1995 southern Hyogo (Kobe) earthquake (M7.3) using double-difference tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318309467264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Multiscaling of shear zones and the evolution of the brittle‐to‐viscous transition in continental crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318898404608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Role of Fluids in Faulting Inferred from Stress Field Signatures"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670319923351680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Local stress concentration in the seismic belt along the Japan Sea coast inferred from precise focal mechanisms: Implications for the stress accumulation process on intraplate earthquake faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320024301568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High-pressure fluid at hypocentral depths in the L'Aquila region inferred from earthquake focal mechanisms"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795302132608","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Implications of fault-valve behaviour for rupture nucleation and recurrence"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269432191488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low‐velocity damaged structure of the San Andreas Fault at Parkfield from fault zone trapped waves"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270627910144","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Detection of small earthquakes with dense array data: example from the San Jacinto fault zone, southern California"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230768768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fracture Strength of the Estimated from Laboratory Experiments: A possibility of high-pressure type fracturing in the crust."},{"@value":"岩石の破壊強度から求められた地殻強度と地殻での高圧型破壊の可能性"},{"@language":"ja-Kana","@value":"ガンセキ ノ ハカイ キョウド カラ モトメラレタ チカク キョウド ト チカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305605632","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地震計アレイ観測に基づく不均質構造の推定"},{"@language":"en","@value":"Imaging of Inhomogeneous Structure Based on Seismic Array Observations"},{"@language":"ja-Kana","@value":"ジシンケイ アレイ カンソク ニ モトヅク フキンシツ コウゾウ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390004222631015424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heterogeneity of Stress Field in NE Japan and Implications for Fault Strength and Earthquake Occurrence Mechanism"},{"@language":"ja","@value":"近年の地震観測により得られた東北日本の応力場の不均質性と断層強度および地震発生機構の関係"},{"@language":"ja-Kana","@value":"キンネン ノ ジシン カンソク ニ ヨリ エラレタ トウホク ニホン ノ オウリョクジョウ ノ フキンシツセイ ト ダンソウ キョウド オヨビ ジシン ハッセイ キコウ ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681215211008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fault rocks in the aftershock area and the neighborhood of 2000 Tottori-ken Seibu earthquake"},{"@language":"ja","@value":"2000年鳥取県西部地震の余震域およびその周辺に分布する断層岩類"},{"@language":"ja-Kana","@value":"2000ネン トットリケン セイブ ジシン ノ ヨシンイキ オヨビ ソノ シュウヘン ニ ブンプ スル ダンソウガンルイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217683072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Comparison of fault gouges in the aftershock area and the non aftershock area of the 2000 Tottori-ken Seibu earthquake"},{"@language":"ja","@value":"2000年鳥取県西部地震の余震域と非余震域に分布する断層ガウジの比較"},{"@language":"ja-Kana","@value":"2000ネン トットリケン セイブ ジシン ノ ヨシンイキ ト ヒヨシンイキ ニ ブンプ スル ダンソウ ガウジ ノ ヒカク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488306432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High resolution 3-D velocity structure in the source region of the 2000 Western Tottori Earthquake in southwestern Honshu, Japan using very dense aftershock observations"},{"@value":"High resolution 3-D velocity structure in the source region of the 2000 Western Tottori Earthquake in the southwestern Honshu, Japan using very dense aftershock observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488738432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-dimensional seismic velocity structure as determined by double-difference tomography in and around the focal area of the 2005 West off Fukuoka Prefecture earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390285697607722624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Overview of the Special Issue “Crustal Dynamics (Part II): Toward the Integration of Geology and Geophysics”"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564227346140416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stress Tensor Inversion Using Seismological Data"},{"@language":"ja","@value":"地震学的データを用いた応力インバージョン"},{"@language":"ja-Kana","@value":"ジシンガクテキ データ オ モチイタ オウリョク インバージョン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390567172584423680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Quaternary Tectonics of Central Kyushu and the 2016 Kumamoto Earthquake: From a Multifaceted Viewpoint Combining Geology, Seismology, and Geodesy"},{"@language":"ja","@value":"九州中部の第四紀テクトニクスと2016年熊本地震"},{"@value":"九州中部の第四紀テクトニクスと2016年熊本地震 : 地質-地震-測地の複眼的視点から"},{"@language":"ja-Kana","@value":"キュウシュウ チュウブ ノ ダイシキ テクトニクス ト 2016ネン クマモト ジシン : チシツ-ジシン-ソクチ ノ フクガンテキ シテン カラ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390567172584438144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Introduction to the Special Issue “Crustal Dynamics (Part II): Toward the Integration of Geology and Geophysics”"},{"@language":"ja","@value":"特集号「地殻ダイナミクス（Part II）—地質学と地球物理学の融合に向けて—」巻頭言"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267021825664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep structure of the Ou mountain range strain concentration zone and the focal area of the 2008 Iwate-Miyagi Nairiku earthquake, NE Japan : seismogenesis related with magma and crustal fluid"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2008067218"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I030621757"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.511"},{"@type":"CIA","@value":"130007921866"},{"@type":"KAKEN","@value":"PRODUCT-23419117"},{"@type":"OPENAIRE","@value":"doi_dedup___::2fa441581a2563c00e0b03c90b5d77cd"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.451_references_DOI_U7L8FpXUA6ofURRnaj6hWbgn25c"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.447_references_DOI_U7L8FpXUA6ofURRnaj6hWbgn25c"},{"@type":"CROSSREF","@value":"10.1146/annurev-earth-040523-120834_references_DOI_U7L8FpXUA6ofURRnaj6hWbgn25c"},{"@type":"CROSSREF","@value":"10.1029/2019gl084841_references_DOI_U7L8FpXUA6ofURRnaj6hWbgn25c"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01186-2_references_DOI_U7L8FpXUA6ofURRnaj6hWbgn25c"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.443_references_DOI_U7L8FpXUA6ofURRnaj6hWbgn25c"}]}