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TitreSeismicity along St. Lawrence paleorift faults overprinted by a meteorite impact structure in Charlevoix, Quebec, eastern Canada
AuteurYu, H; Liu, Y; Harrington, R M; Lamontagne, M
SourceBulletin of the Seismological Society of America vol. 106, 6, 2016 p. 2663-2673, https://doi.org/10.1785/0120160036
Année2016
Séries alt.Ressources naturelles Canada, Contribution externe 20182448
ÉditeurSeismological Society of America
Documentpublication en série
Lang.anglais
DOIhttps://doi.org/10.1785/0120160036
Mediapapier; en ligne; numérique
ProgrammeRisques géologique du tremblement de terre, Géoscience pour la sécurité publique
Diffusé2016 09 20
Résumé(disponible en anglais seulement)
The Charlevoix seismic zone (CSZ) in Qubec has the highest number of earthquakes in eastern Canada, with cataloged events diffusely distributed between the St. Lawrence paleorift faults. In this study, we relocate 1242 out of 1639 earthquakes in the CSZ from 1988 to 2010 using double-difference relocations with phase arrivals from manual picks and waveform cross correlations and requiring a strict set of quality control criteria. Our results show a diffuse distribution of earthquakes beneath the St. Lawrence River within a meteorite impact structure and clear lineations of event hypocenters outside the inner boundary of the impact structure. The diffuse seismicity distribution coupled with a lower cumulative seismic moment within the impact structure, despite a higher number of events, suggests the presence of highly fractured crust and weakened pre-existing faults. A lack of MN ³4:0 earthquakes and a wide variation of focal mechanism P-axis orientations also provide evidence for weakened preexisting faults. Relocated earthquakes beneath the north shore of the St. Lawrence River illuminate a broad southeast-trending linear structure, suggesting the geometry of the Gouffre northwest River fault. A paucity of seismicity between the north shore and the river may correspond to fault-controlled basins of unconsolidated sediments at the surface and volumes of high-seismic-velocity material at midcrustal depths. © 2016, Seismological Society of America. All rights reserved.
GEOSCAN ID311039