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001	9.959236
003	CaOODSP
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007	cr |n|||||||||
008	260123t20162016oncb    ob   f|0| 0 eng d
040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-qu
086	1 |aM183-2/7945E-PDF
100	1 |aBent, Allison Lyn, |eauthor.
245	10|aMagnitude conversion relations for very short distances : |bthe Charlevoix, Quebec, Seismic Zone / |cA.L. Bent and F. Vadnais.
264	1|a[Ottawa] : |bGeological Survey of Canada, |c2016.
264	4|c©2016
300	|a1 online resource (17 pages) : |bcharts, maps.
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aOpen file, |x2816-7155 ; |v7945
504	|aIncludes bibliographical references (pages 8-9).
520	|a"The Charlevoix Seismic Zone northeast of Quebec City is one of the most active seismic zones in eastern Canada and the seismograph station density is higher than in most other regions of eastern Canada. These two factors combined make it an ideal region for comparing earthquakes of different magnitudes and for comparing the same earthquake at local and regional distances. Using data from the Charlevoix region we develop magnitude conversion relations between magnitudes recorded at distances of less than 50 km and the standard MN magnitude based on the Lg phase"--Introduction, page 4.
650	0|aEarthquake magnitude|zQuébec (Province)|zCharlevoix Region.
650	6|aTremblements de terre|xMagnitude|zQuébec (Province)|zCharlevoix (Région)
710	2 |aGeological Survey of Canada, |eissuing body.
830	#0|aOpen file (Geological Survey of Canada)|v7945.|w(CaOODSP)9.506878
856	40|qPDF|s0.98 MB|uhttps://publications.gc.ca/collections/collection_2026/rncan-nrcan/m183-2/M183-2-7945-eng.pdf
856	4 |qHTML|sN/A|uhttps://doi.org/10.4095/297964