Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data ...
Models of seismic velocity structure of the crust in the seismically active northern Canadian Cordillera remain poorly constrained, despite their importance in the accurate location and characterization of regional earthquakes. On 29 August 2014, a moderate earthquake with magnitude MB 5.0 occurred...
| Main Authors: | , |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
My University
2017
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.20381/ruor-20431 https://ruor.uottawa.ca/handle/10393/36151 |
| Summary: | Models of seismic velocity structure of the crust in the seismically active northern Canadian Cordillera remain poorly constrained, despite their importance in the accurate location and characterization of regional earthquakes. On 29 August 2014, a moderate earthquake with magnitude MB 5.0 occurred in the Northwest Territories, Canada, ~100 km to the east of the Cordilleran Deformation Front, which generated high-quality Rayleigh wave data. We carefully selected 23 seismic stations that recorded the Rayleigh waves and divided them into 13 groups according to the azimuth angle between the earthquake and the stations; these groups mostly sample the Cordillera. In each group, we measured Rayleigh wave group velocity dispersion, which we inverted for one-dimensional shear-wave velocity models of the crust. We thus obtained 13 models that consistently show low seismic velocities with respect to reference models, with a slow upper and lower crust surrounding a relatively fast mid crustal layer. The average of the ... |
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