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...
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Online Access: | http://hdl.handle.net/10393/36151 https://doi.org/10.1139/cjes-2016-0115 |
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ftunivottawa:oai:ruor.uottawa.ca:10393/36151 2023-05-15T17:46:42+02:00 Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data Ma, Shutian Audet, Pascal 2017 application/pdf http://hdl.handle.net/10393/36151 https://doi.org/10.1139/cjes-2016-0115 en eng Canadian Journal of Earth Sciences 54(2) 0008-4077 http://hdl.handle.net/10393/36151 doi:10.1139/cjes-2016-0115 2017 ftunivottawa https://doi.org/10.1139/cjes-2016-0115 2021-01-04T18:26:57Z 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 13 models is consistent with receiver function data in the central portion of the Cordillera. Finally, we compare earthquake locations determined by the Geological Survey of Canada using a simple homogenous crust over a mantle half space with those estimated using the new crustal velocity model, and show that estimates can differ by as much as 10 km. Other/Unknown Material Northwest Territories uO Research (University of Ottawa - uOttawa) Canada Northwest Territories Canadian Journal of Earth Sciences 54 2 163 172 |
institution |
Open Polar |
collection |
uO Research (University of Ottawa - uOttawa) |
op_collection_id |
ftunivottawa |
language |
English |
description |
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 13 models is consistent with receiver function data in the central portion of the Cordillera. Finally, we compare earthquake locations determined by the Geological Survey of Canada using a simple homogenous crust over a mantle half space with those estimated using the new crustal velocity model, and show that estimates can differ by as much as 10 km. |
author |
Ma, Shutian Audet, Pascal |
spellingShingle |
Ma, Shutian Audet, Pascal Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data |
author_facet |
Ma, Shutian Audet, Pascal |
author_sort |
Ma, Shutian |
title |
Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data |
title_short |
Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data |
title_full |
Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data |
title_fullStr |
Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data |
title_full_unstemmed |
Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data |
title_sort |
seismic velocity model of the crust in the northern canadian cordillera from rayleigh wave dispersion data |
publishDate |
2017 |
url |
http://hdl.handle.net/10393/36151 https://doi.org/10.1139/cjes-2016-0115 |
geographic |
Canada Northwest Territories |
geographic_facet |
Canada Northwest Territories |
genre |
Northwest Territories |
genre_facet |
Northwest Territories |
op_relation |
Canadian Journal of Earth Sciences 54(2) 0008-4077 http://hdl.handle.net/10393/36151 doi:10.1139/cjes-2016-0115 |
op_doi |
https://doi.org/10.1139/cjes-2016-0115 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
54 |
container_issue |
2 |
container_start_page |
163 |
op_container_end_page |
172 |
_version_ |
1766150496829046784 |