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• W4291718368 abstract "PreviousNext No AccessSecond International Meeting for Applied Geoscience & EnergyInterferometry derived S-wave velocity model with geological constrains for induced seismicity monitoringAuthors: Galina SimeonovaDmitry AlexandrovToufik ChtoukiPetr KolínskýLeo EisnerTijmen Jan MoserUmair WaheedSherif HanafyBarbara CoxGalina SimeonovaSeismikSearch for more papers by this author, Dmitry AlexandrovSeismikSearch for more papers by this author, Toufik ChtoukiSeismikSearch for more papers by this author, Petr KolínskýInstitute of GeophysicsSearch for more papers by this author, Leo EisnerSeismikSearch for more papers by this author, Tijmen Jan MoserSeismikSearch for more papers by this author, Umair WaheedCPG KFUPMSearch for more papers by this author, Sherif HanafyCPG KFUPMSearch for more papers by this author, and Barbara CoxHydrecoGeomecSearch for more papers by this authorhttps://doi.org/10.1190/image2022-3745723.1 SectionsSupplemental MaterialAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InRedditEmail AbstractBoth P-wave and S-wave velocity models are needed for location of induced seismicity from sparse monitoring arrays. While P-waves are usually known (reflection surveys or sonic logs), S-wave models need additional constrains. We use seismic noise interferometry to obtain Rayleigh surface waves between receivers of the sparse array. We invert the Rayleigh wave dispersion curves for the S-wave velocity structure beneath the array with additional constrains on layer boundaries derived from the P-wave model. An application on a sparse array in urban environment in The Hague, The Netherlands, reveals very low S-wave velocities in the near surface layers and S-wave increase with depth. Both of these observations are consistent with unconsolidated sediments and S-wave velocities observed in other parts of the Netherlands (Groningen).Keywords: interferometry, microseismicity, induced sesimicity, velocity model building, surface wavesPermalink: https://doi.org/10.1190/image2022-3745723.1FiguresReferencesRelatedDetails Second International Meeting for Applied Geoscience & EnergyISSN (print):1052-3812 ISSN (online):1949-4645Copyright: 2022 Pages: 3694 publication data© 2022 Published in electronic format with permission by the Society of Exploration Geophysicists and the American Association of Petroleum GeologistsPublisher:Society of Exploration Geophysicists HistoryPublished Online: 15 Aug 2022 CITATION INFORMATION Galina Simeonova, Dmitry Alexandrov, Toufik Chtouki, Petr Kolínský, Leo Eisner, Tijmen Jan Moser, Umair Waheed, Sherif Hanafy, and Barbara Cox, (2022), Interferometry derived S-wave velocity model with geological constrains for induced seismicity monitoring, SEG Technical Program Expanded Abstracts : 1556-1560. https://doi.org/10.1190/image2022-3745723.1 Plain-Language Summary Keywordsinterferometrymicroseismicityinduced sesimicityvelocity model buildingsurface wavesPDF DownloadLoading ..." @default.
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• W4291718368 date "2022-08-15" @default.
• W4291718368 modified "2023-09-27" @default.
• W4291718368 title "Interferometry derived S-wave velocity model with geological constrains for induced seismicity monitoring" @default.
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• W4291718368 doi "https://doi.org/10.1190/image2022-3745723.1" @default.
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