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001	9.959739
003	CaOODSP
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006	m     o  d f
007	cr |n|||||||||
008	260210t20162016oncdb   ob   f|0| 0 eng d
040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-bc
086	1 |aM183-2/8030E-PDF
100	1 |aFarahbod, A. M., |eauthor.
245	10|aSeismic attenuation in the Anahim Volcanic Belt and adjacent regions of British Columbia / |cA.M. Farahbod and J.F. Cassidy.
264	1|a[Ottawa] : |bGeological Survey of Canada, |c2016.
264	4|c©2016
300	|a1 online resource (50 pages) : |bcharts, maps.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aOpen file, |x2816-7155 ; |v8030
504	|aIncludes bibliographical references (pages 22-23).
520	|a"In this study we investigated coda-wave attenuation (Qc) in the interior of British Columbia, with a focus on the Anahim Volcanic Belt (AVB) and specifically the Nazko Cone region using the single scattering approximation on records from short period and broadband stations of the regional Canadian National Seismic Network (CNSN) and POLARIS Network. Our dataset is comprised of 380 earthquakes recorded between 1999 and 2012 with magnitudes ranging from 1.6 to 3.9, depths from 0 to 36 km and epicentral distances of 15 to 100 km. This gives a total of 423 high signal to noise (S/N) traces (S/N≥5.0) useful for Qc calculation (with a range of ellipse parameter, a2, of 30 to 110) across the region"--Abstract, page 4.
650	0|aSeismic waves|zBritish Columbia|xScattering.
650	6|aOndes sismiques|zColombie-Britannique|xDiffusion.
710	2 |aGeological Survey of Canada, |eissuing body.
830	#0|aOpen file (Geological Survey of Canada)|v8030.|w(CaOODSP)9.506878
856	40|qPDF|s2.80 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-8030-eng.pdf
856	4 |qHTML|sN/A|uhttps://doi.org/10.4095/306590