Seismic Activation Model Reconciliation (submitted to KeAI Earthquake Science)

dc.contributor.authorBrox, Daniel
dc.date.accessioned2025-11-15T03:54:13Z
dc.date.issued2025-11-15
dc.description.abstractA strain energy diffusion model is presented as a means of reconciling different seismic moment time scaling relations presented by previous seismic activation models. Using similarity solutions to the 1D modified porous medium equation, anomalous diffusion of strain energy along the mainshock fault is demonstrated to increase strain energy density at the mainshock hypocenter while decreasing strain energy density elsewhere until mainshock rupture occurs.
dc.description.provenanceSubmitted by Daniel Brox (dbrox@ece.ubc.ca) on 2025-11-15T03:54:13Z No. of bitstreams: 1 RGbasics.pdf: 657448 bytes, checksum: 02bad30b9d02bf9ed06206925fedbd37 (MD5)en
dc.description.provenanceMade available in DSpace on 2025-11-15T03:54:13Z (GMT). No. of bitstreams: 1 RGbasics.pdf: 657448 bytes, checksum: 02bad30b9d02bf9ed06206925fedbd37 (MD5) Previous issue date: 2025-11-15en
dc.identifier.urihttps://africarxiv.ubuntunet.net/handle/1/10574
dc.language.isoen
dc.titleSeismic Activation Model Reconciliation (submitted to KeAI Earthquake Science)
dc.typeArticle

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