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Ground motions of the december 2015 M 4.7 Vancouver Island earthquake; attenuation and site response

Frederick Jackson, Sheri Molnar, Hadi Ghofrani, Gail M. Atkinson, John F. Cassidy and Karen Assatourians
Ground motions of the december 2015 M 4.7 Vancouver Island earthquake; attenuation and site response
Bulletin of the Seismological Society of America (December 2017) 107 (6): 2903-2916

Abstract

The December 2015 moment magnitude (M) 4.7 Vancouver Island earthquake is one of the largest recorded inslab earthquakes within Georgia Strait, British Columbia, Canada. Ground motions from all seismic stations within 500 km from the epicenter are examined. Peak ground acceleration reached a maximum of 4.65%g in Greater Victoria. We compare the observed horizontal-component 5% damped pseudospectral acceleration (PSA) values with the inslab ground-motion prediction equation (GMPE) suite used in the 2015 National Building Code of Canada (NBCC). PSA values from this event are significantly lower than the expected 2015 NBCC values for an M 4.7 inslab event, highlighting poor GMPE scaling at this low magnitude level. We develop an event-specific GMPE to constrain the source and attenuation parameters in comparison with seismological models. Potential site effects are examined at strong-motion stations within 85 km of the epicenter. High amplification at 4-6 Hz is observed on both thick sediment sites and on the northern edge of the Fraser delta, as observed in previous earthquakes. Gross generalizations of observed variable earthquake shaking are captured by current regional seismic microzonation maps; however, local discrepancies are present. This earthquake generated the first borehole array recordings obtained at depth in British Columbia. Recorded motions increase toward the surface and are of similar or higher amplitude than at nearby surface stations. Amplification between top and bottom sensors is a consistent factor of 7-8 in all three arrays over a similar 40-45-m depth interval of Fraser delta sediments. Cross-correlation analysis determines shear-wave velocity estimates less than 350 m/s consistent with these delta sediments.


ISSN: 0037-1106
EISSN: 1943-3573
Coden: BSSAAP
Serial Title: Bulletin of the Seismological Society of America
Serial Volume: 107
Serial Issue: 6
Title: Ground motions of the december 2015 M 4.7 Vancouver Island earthquake; attenuation and site response
Affiliation: University of Western Ontario, Department of Earth Sciences, London, ON, United States
Pages: 2903-2916
Published: 201712
Text Language: English
Publisher: Seismological Society of America, Berkeley, CA, United States
References: 40
Accession Number: 2018-031658
Categories: Seismology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 2 tables, sketch maps
N46°00'00" - N52°00'00", W125°00'00" - W120°00'00"
Secondary Affiliation: Canadian Geological Survey, CAN, Canada
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2018, American Geosciences Institute. Abstract, Copyright, Seismological Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 2018
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