FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2057422021> ?p ?o ?g. }

• W2057422021 endingPage "85" @default.
• W2057422021 startingPage "74" @default.
• W2057422021 abstract "Research Article| January 01, 1997 Stochastic Point-Source Modeling of Ground Motions in the Cascadia Region Gail M. Atkinson; Gail M. Atkinson Department of Earth Sciences Carleton University Ottawa, Ont. K1S 5B6 (613) 623-3240 (phone and FAX) email: gma@ccs.carleton.ca (G.M.A.) Search for other works by this author on: GSW Google Scholar David M. Boore David M. Boore U.S. Geological Survey 345 Middlefield Rd. Menlo Park, Ca. 94025 (415) 329-5616 email: boore@somoa.wr.usgs.gov (D.M.B.) Search for other works by this author on: GSW Google Scholar Seismological Research Letters (1997) 68 (1): 74–85. https://doi.org/10.1785/gssrl.68.1.74 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Gail M. Atkinson, David M. Boore; Stochastic Point-Source Modeling of Ground Motions in the Cascadia Region. Seismological Research Letters 1997;; 68 (1): 74–85. doi: https://doi.org/10.1785/gssrl.68.1.74 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search Abstract A stochastic model is used to develop preliminary ground motion relations for the Cascadia region for rock sites. The model parameters are derived from empirical analyses of seismographic data from the Cascadia region. The model is based on a Brune point-source characterized by a stress parameter of 50 bars. The model predictions are compared to ground-motion data from the Cascadia region and to data from large earthquakes in other subduction zones. The point-source simulations match the observations from moderate events (M < 7) in the Cascadia region. The simulations predict a steeper attenuation than observed for very large subduction events (M > 7.5) in other regions; motions are overpredicted near the earthquake source and underpredicted at large distances (> 100 km). The discrepancy at large magnitudes suggests further work on modeling finite-fault effects and regional attenuation is warranted. In the meantime, the preliminary equations are satisfactory for predicting motions from events of M < 7 and provide conservative estimates of motions from larger events at distances less than 100 km. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2057422021 created "2016-06-24" @default.
• W2057422021 creator A5030723338 @default.
• W2057422021 creator A5040811104 @default.
• W2057422021 date "1997-01-01" @default.
• W2057422021 modified "2023-10-08" @default.
• W2057422021 title "Stochastic Point-Source Modeling of Ground Motions in the Cascadia Region" @default.
• W2057422021 cites W1819897745 @default.
• W2057422021 cites W1994553199 @default.
• W2057422021 cites W2092579927 @default.
• W2057422021 cites W2099566008 @default.
• W2057422021 cites W2105658614 @default.
• W2057422021 cites W2110114457 @default.
• W2057422021 cites W2140618997 @default.
• W2057422021 cites W2146244083 @default.
• W2057422021 cites W2157939761 @default.
• W2057422021 cites W2164278512 @default.
• W2057422021 cites W2185410891 @default.
• W2057422021 cites W2207305543 @default.
• W2057422021 cites W2268937280 @default.
• W2057422021 cites W2286620461 @default.
• W2057422021 cites W2561460856 @default.
• W2057422021 cites W2754819143 @default.
• W2057422021 doi "https://doi.org/10.1785/gssrl.68.1.74" @default.
• W2057422021 hasPublicationYear "1997" @default.
• W2057422021 type Work @default.
• W2057422021 sameAs 2057422021 @default.
• W2057422021 citedByCount "74" @default.
• W2057422021 countsByYear W20574220212012 @default.
• W2057422021 countsByYear W20574220212013 @default.
• W2057422021 countsByYear W20574220212014 @default.
• W2057422021 countsByYear W20574220212015 @default.
• W2057422021 countsByYear W20574220212016 @default.
• W2057422021 countsByYear W20574220212017 @default.
• W2057422021 countsByYear W20574220212018 @default.
• W2057422021 countsByYear W20574220212019 @default.
• W2057422021 countsByYear W20574220212020 @default.
• W2057422021 countsByYear W20574220212021 @default.
• W2057422021 countsByYear W20574220212022 @default.
• W2057422021 countsByYear W20574220212023 @default.
• W2057422021 crossrefType "journal-article" @default.
• W2057422021 hasAuthorship W2057422021A5030723338 @default.
• W2057422021 hasAuthorship W2057422021A5040811104 @default.
• W2057422021 hasConcept C127313418 @default.
• W2057422021 hasConcept C136764020 @default.
• W2057422021 hasConcept C161191863 @default.
• W2057422021 hasConcept C166957645 @default.
• W2057422021 hasConcept C199360897 @default.
• W2057422021 hasConcept C205649164 @default.
• W2057422021 hasConcept C23123220 @default.
• W2057422021 hasConcept C2524010 @default.
• W2057422021 hasConcept C2778447006 @default.
• W2057422021 hasConcept C2778805511 @default.
• W2057422021 hasConcept C2780154274 @default.
• W2057422021 hasConcept C28719098 @default.
• W2057422021 hasConcept C33923547 @default.
• W2057422021 hasConcept C41008148 @default.
• W2057422021 hasConceptScore W2057422021C127313418 @default.
• W2057422021 hasConceptScore W2057422021C136764020 @default.
• W2057422021 hasConceptScore W2057422021C161191863 @default.
• W2057422021 hasConceptScore W2057422021C166957645 @default.
• W2057422021 hasConceptScore W2057422021C199360897 @default.
• W2057422021 hasConceptScore W2057422021C205649164 @default.
• W2057422021 hasConceptScore W2057422021C23123220 @default.
• W2057422021 hasConceptScore W2057422021C2524010 @default.
• W2057422021 hasConceptScore W2057422021C2778447006 @default.
• W2057422021 hasConceptScore W2057422021C2778805511 @default.
• W2057422021 hasConceptScore W2057422021C2780154274 @default.
• W2057422021 hasConceptScore W2057422021C28719098 @default.
• W2057422021 hasConceptScore W2057422021C33923547 @default.
• W2057422021 hasConceptScore W2057422021C41008148 @default.
• W2057422021 hasIssue "1" @default.
• W2057422021 hasLocation W20574220211 @default.
• W2057422021 hasOpenAccess W2057422021 @default.
• W2057422021 hasPrimaryLocation W20574220211 @default.
• W2057422021 hasRelatedWork W1504514227 @default.
• W2057422021 hasRelatedWork W2056060060 @default.
• W2057422021 hasRelatedWork W2076882245 @default.
• W2057422021 hasRelatedWork W2175435306 @default.
• W2057422021 hasRelatedWork W220677501 @default.
• W2057422021 hasRelatedWork W2981902742 @default.
• W2057422021 hasRelatedWork W3175319091 @default.
• W2057422021 hasRelatedWork W4207071872 @default.
• W2057422021 hasRelatedWork W4283720006 @default.
• W2057422021 hasRelatedWork W4360922125 @default.
• W2057422021 hasVolume "68" @default.
• W2057422021 isParatext "false" @default.
• W2057422021 isRetracted "false" @default.
• W2057422021 magId "2057422021" @default.
• W2057422021 workType "article" @default.