000 01870cam  2200301za 4500
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008180323s2018    oncbd   obs  f000 0 eng d
040 |aCaOODSP|beng
043 |an-cn-ab|an-cn-bc
0861 |aM183-2/8221E-PDF
1001 |aFarahbod, A. M.
24510|aSeismic attenuation in the interior of British Columbia and westernmost continental craton |h[electronic resource] / |cA.M. Farahbod and J.F. Cassidy.
260 |a[Ottawa] : |bNatural Resources Canada, |c2018.
300 |a68 p. : |bcharts (some col.), col. maps.
4901 |aOpen file ; |v8221
504 |aIncludes bibliographical references (p. 22-23).
520 |a“This study examines seismic attenuation across western Canada in a wide range of tectonic environments - from an active subduction zone in the west, through a volcanic belt, to the stable craton in the east. We determine a clear link between the attenuation patterns, the tectonic setting, and the seismicity rate - with the greatest attenuation in the most seismically active regions, and the lowest attenuation on the stable craton. Our research helps to constrain the boundaries of various tectonic environments across western Canada, and provides new details on the seismic attenuation - both of which will contribute to improved earthquake and volcanic hazard models for this region”--Provided by publisher.
69207|2gccst|aSeismology
69207|2gccst|aEarthquakes
693 4|aSeismic waves
7001 |aCassidy, John Francis, |d1959-
7101 |aCanada. |bNatural Resources Canada.
7102 |aGeological Survey of Canada.
830#0|aOpen file (Geological Survey of Canada)|v8221.|w(CaOODSP)9.506878
85640|qPDF|s4.08 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-2/M183-2-8221-eng.pdf