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TitreSeismic hazard in western Canada from global positioning system strain rate data
AuteurLeonard, L J; Mazzotti, S; Cassidy, J F; Rogers, G; Halchuk, S
SourceProceedings of the 9th U.S. National and 10th Canadian Conference on Earthquake Engineering/Compte Rendu de la 9ième Conférence Nationale Américaine et 10ième Conférence Canadienne de Génie Parasismique; 753, 2010, 10 pages
Séries alt.Secteur des sciences de la Terre, Contribution externe 20090278
Réunion10th Canadian Conference / 9th US Conference on Earthquake Engineering; Toronto, ON; CA; juillet 25-29, 2010
Référence reliéeCette publication est contenue dans Adams, J; Halchuk, S; Awatta, A; Adams, J; Halchuk, S; Awatta, A; (2010). Estimated seismic design values for Canadian missions abroad, Proceedings of the 9th U.S. National and 10th Canadian Conference on Earthquake Engineering
SNRC82E; 82F; 82G; 82J; 82K; 82L; 82M; 82N; 83D; 92; 93; 94B; 94C; 94D; 94E; 94F; 94K; 94L; 94M; 102; 103; 104
Lat/Long OENS-140.0000 -114.0000 60.0000 48.0000
Sujetssecousses séismiques; risque de tremblement de terre; études séismiques; magnitudes des séismes; géophysique
Illustrationslocation maps; plots
ProgrammeÉvaluations ciblées des dangers dans l'Ouest du Canada, Géoscience pour la sécurité publique
Résumé(disponible en anglais seulement)
Probabilistic seismic hazard analyses are principally based on frequency magnitude statistics of historical and instrumental earthquake catalogues. This method assumes that return periods of large damaging earthquakes (100s-1000s yr) can be extrapolated from 50-100 yr statistics of small and medium earthquakes. The method has obvious limitations when applied to areas of low level seismicity where the earthquake statistics may be poorly constrained. In this study, we test an alternative approach to assess seismic hazard in Western Canada. We use horizontal velocities at ~250 Global Positioning System (GPS) sites in BC and Alberta to calculate strain rates and earthquake statistics within seismic source zones. GPS-based strain rates are converted to seismic moment, earthquake frequency-magnitude statistics, and seismic hazard using a logic-tree method. The GPS-based earthquake statistics and seismic hazard are then compared to those derived from the earthquake catalogue. In one zone (Puget Sound), the GPS seismic hazard estimates are in good agreement with those from earthquake statistics. In nearly all other zones (e.g., most of BC and Alberta), the GPS seismic hazard estimates are significantly larger than those from the earthquake catalogue by one or two orders of magnitude. This discrepancy could indicate that the earthquake catalogue significantly under predicts long-term seismic hazard (over 100s-1000s yr) in areas of low-level seismicity. Alternatively, significant aseismic deformation may occur over long time-scales, which would imply that the GPS strain rates over predict the true seismic hazard. We discuss the nature and limitations of both methods in light of our results for Western Canada, with the goal of defining a methodology to incorporate GPS strain rate data into probabilistic seismic hazard assessments.