FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3215431750> ?p ?o ?g. }

• W3215431750 abstract "PreviousNext No AccessProceedings of the 14th SEGJ International Symposium, Online, 18–21 October 2021Three-dimensional S-wave velocity structure of the Kinki Region, southwestern Japan with ambient seismic noise tomography using a dense seismic arrayAuthors: Bokani NthabaTatsunori IkedaTakeshi TsujiHiro NimiyaYoshihisa IioBokani NthabaDepartment of Earth Resources Engineering, Kyushu UniversityEarth and Environmental Sciences Department, Botswana International University of Science and TechnologySearch for more papers by this author, Tatsunori IkedaDepartment of Earth Resources Engineering, Kyushu UniversitySearch for more papers by this author, Takeshi TsujiDepartment of Earth Resources Engineering, Kyushu UniversityInternational Institute for Carbon-Neutral Energy Research, Kyushu UniversitySearch for more papers by this author, Hiro NimiyaDepartment of Earth Resources Engineering, Kyushu UniversityAISTSearch for more papers by this author, and Yoshihisa IioDisaster Prevention Research Institute, Kyoto UniversitySearch for more papers by this authorhttps://doi.org/10.1190/segj2021-067.1 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail Abstract Research interest in the Kinki region, southwestern Japan, has been aroused by the frequent occurrence of microearthquake activity in the area, particularly on the northern side of the Arima-Takatsuki Tectonic Line. Previous studies targeting this area focused mainly on deep, large-scale structures and could not efficiently resolve fine-scale shallow crustal structures, hence the need for an improved spatial resolution characterization of the upper crustal structure of this region. By cross-correlating the vertical components of the continuous ambient seismic noise data recorded between April 1st and September 30th, 2019, we estimated phase velocities using a frequency domain method to construct the three-dimensional S-wave velocity model of the Kinki region. We used data recorded by the dense Hi-net high-sensitivity seismographs and the Manten seismic network administered by Kyoto University, AIST, NIED, and the JMA. Rayleigh wave dispersion data were determined from zero crossings of the real component of the cross spectra using Aki’s spectral formulation, and a direct surface-wave inversion method was utilized to estimate the 3D S-wave velocity structure. This study revealed a low-velocity tectonic structure coinciding with the location of the reactivated Niigata-Kobe Tectonic Zone coexisting with fine-scale low-velocity tectonic structures on its flanks, which are likely to be indicating active fault locations. Additionally, these results indicate the presence of high-velocity zones on the northwestern and the southeastern portions of the study area attributable to very shallow basement material, mountainous regions, or sedimentary complexes. Sedimentary basins manifest as low-velocity zones extending to depths of about 2.2 km. These results contribute to deepening fundamental discerning of earthquake faulting and will be useful in hazard assessment and disaster mitigation. Keywords: ambient noise, Kinki region, Niigata-Kobe tectonic zone, zero crossing method, direct surface-wave inversion, Manten seismic networkPermalink: https://doi.org/10.1190/segj2021-067.1FiguresReferencesRelatedDetails Proceedings of the 14th SEGJ International Symposium, Online, 18–21 October 2021ISSN (online):2159-6832Copyright: 2021 Pages: 349 publication data© 2021 Published in electronic format with permission by the Society of Exploration Geophysicists of JapanPublisher:Society of Exploration GeophysicistsSociety of Exploration Geophysicists of Japan HistoryPublished Online: 29 Nov 2021 CITATION INFORMATION Bokani Nthaba, Tatsunori Ikeda, Takeshi Tsuji, Hiro Nimiya, and Yoshihisa Iio, (2021), Three-dimensional S-wave velocity structure of the Kinki Region, southwestern Japan with ambient seismic noise tomography using a dense seismic array, SEG Global Meeting Abstracts : 252-255. https://doi.org/10.1190/segj2021-067.1 Plain-Language Summary Keywordsambient noiseKinki regionNiigata-Kobe tectonic zonezero crossing methoddirect surface-wave inversionManten seismic networkPDF DownloadLoading ..." @default.
• W3215431750 created "2021-12-06" @default.
• W3215431750 creator A5040472136 @default.
• W3215431750 creator A5045770756 @default.
• W3215431750 creator A5061737731 @default.
• W3215431750 creator A5065322660 @default.
• W3215431750 creator A5091910194 @default.
• W3215431750 date "2021-11-29" @default.
• W3215431750 modified "2023-09-23" @default.
• W3215431750 title "Three-dimensional S-wave velocity structure of the Kinki Region, southwestern Japan with ambient seismic noise tomography using a dense seismic array" @default.
• W3215431750 cites W1991394204 @default.
• W3215431750 cites W2021775323 @default.
• W3215431750 cites W2028843000 @default.
• W3215431750 cites W2029660105 @default.
• W3215431750 cites W2061777253 @default.
• W3215431750 cites W2075130232 @default.
• W3215431750 cites W2132342875 @default.
• W3215431750 cites W2466771544 @default.
• W3215431750 cites W2614378840 @default.
• W3215431750 cites W2778193286 @default.
• W3215431750 cites W2922605165 @default.
• W3215431750 cites W4312827208 @default.
• W3215431750 doi "https://doi.org/10.1190/segj2021-067.1" @default.
• W3215431750 hasPublicationYear "2021" @default.
• W3215431750 type Work @default.
• W3215431750 sameAs 3215431750 @default.
• W3215431750 citedByCount "0" @default.
• W3215431750 crossrefType "proceedings-article" @default.
• W3215431750 hasAuthorship W3215431750A5040472136 @default.
• W3215431750 hasAuthorship W3215431750A5045770756 @default.
• W3215431750 hasAuthorship W3215431750A5061737731 @default.
• W3215431750 hasAuthorship W3215431750A5065322660 @default.
• W3215431750 hasAuthorship W3215431750A5091910194 @default.
• W3215431750 hasConcept C114793014 @default.
• W3215431750 hasConcept C115961682 @default.
• W3215431750 hasConcept C122959257 @default.
• W3215431750 hasConcept C127313418 @default.
• W3215431750 hasConcept C154945302 @default.
• W3215431750 hasConcept C165205528 @default.
• W3215431750 hasConcept C195501115 @default.
• W3215431750 hasConcept C203718221 @default.
• W3215431750 hasConcept C205312793 @default.
• W3215431750 hasConcept C2777084502 @default.
• W3215431750 hasConcept C2993808335 @default.
• W3215431750 hasConcept C30947920 @default.
• W3215431750 hasConcept C41008148 @default.
• W3215431750 hasConcept C67236022 @default.
• W3215431750 hasConcept C77928131 @default.
• W3215431750 hasConcept C78542244 @default.
• W3215431750 hasConcept C8058405 @default.
• W3215431750 hasConcept C83176761 @default.
• W3215431750 hasConcept C99498987 @default.
• W3215431750 hasConceptScore W3215431750C114793014 @default.
• W3215431750 hasConceptScore W3215431750C115961682 @default.
• W3215431750 hasConceptScore W3215431750C122959257 @default.
• W3215431750 hasConceptScore W3215431750C127313418 @default.
• W3215431750 hasConceptScore W3215431750C154945302 @default.
• W3215431750 hasConceptScore W3215431750C165205528 @default.
• W3215431750 hasConceptScore W3215431750C195501115 @default.
• W3215431750 hasConceptScore W3215431750C203718221 @default.
• W3215431750 hasConceptScore W3215431750C205312793 @default.
• W3215431750 hasConceptScore W3215431750C2777084502 @default.
• W3215431750 hasConceptScore W3215431750C2993808335 @default.
• W3215431750 hasConceptScore W3215431750C30947920 @default.
• W3215431750 hasConceptScore W3215431750C41008148 @default.
• W3215431750 hasConceptScore W3215431750C67236022 @default.
• W3215431750 hasConceptScore W3215431750C77928131 @default.
• W3215431750 hasConceptScore W3215431750C78542244 @default.
• W3215431750 hasConceptScore W3215431750C8058405 @default.
• W3215431750 hasConceptScore W3215431750C83176761 @default.
• W3215431750 hasConceptScore W3215431750C99498987 @default.
• W3215431750 hasLocation W32154317501 @default.
• W3215431750 hasOpenAccess W3215431750 @default.
• W3215431750 hasPrimaryLocation W32154317501 @default.
• W3215431750 hasRelatedWork W2004295136 @default.
• W3215431750 hasRelatedWork W2011912193 @default.
• W3215431750 hasRelatedWork W2190900199 @default.
• W3215431750 hasRelatedWork W2801640435 @default.
• W3215431750 hasRelatedWork W2981851802 @default.
• W3215431750 hasRelatedWork W3030244662 @default.
• W3215431750 hasRelatedWork W3092585322 @default.
• W3215431750 hasRelatedWork W3215431750 @default.
• W3215431750 hasRelatedWork W4309479304 @default.
• W3215431750 hasRelatedWork W4360991115 @default.
• W3215431750 isParatext "false" @default.
• W3215431750 isRetracted "false" @default.
• W3215431750 magId "3215431750" @default.
• W3215431750 workType "article" @default.