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| 01881cam 2200337za 4500 |
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| 001 | 9.852469 |
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| 003 | CaOODSP |
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| 005 | 20221107154606 |
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| 007 | cr ||||||||||| |
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| 008 | 180227s1995 onca #o f000 0 eng d |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn-nf |
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| 086 | 1 |aM183-2/3043E-PDF |
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| 100 | 1 |aAdams, John. |
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| 245 | 10|aRevised seismicity of the Grand Banks and offshore Newfoundland |h[electronic resource] / |cJohn Adams and Rutger Wahlström. |
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| 260 | |a[Ottawa] : |bGeological Survey of Canada, |c1995. |
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| 300 | |a58 p. : |bill. |
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| 490 | 1 |aOpen file ; |v3043 |
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| 500 | |aCover title. |
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| 500 | |a"23 March 1995." |
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| 504 | |aIncludes bibliographical references. |
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| 520 | 3 |aA comprehensive reivew of the catalogued seismicity of the Grand Banks of Newfoundland (1922-1994) has revised or added earthquakes in four time periods: 1922-1970, the two largest earthquakes (M≈5) relocated to Baffin Island (1992) and the northern Labrador Sea (1962); 1977-1982, added four new earthquakes; 1969-1984, revised the locations and magnitudes for five earthquakes; 1984-1994, added 15 earthquakes. Many earthquakes appear to be spatially associated with Mesozoic extensional structures that trend northeastwards across the Grand Banks. A cluster of six pos-1970 earthquakes lies 40-80 km northwest of the Hibernia oilfield and represents the most seismically active region of the Grand Banks. |
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| 546 | |aIncludes abstract in French. |
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| 692 | 07|2gccst|aEarthquakes |
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| 692 | 07|2gccst|aSeismology |
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| 700 | 1 |aWahlström, Rutger. |
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| 710 | 1 |aCanada. |bNatural Resources Canada. |
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| 710 | 2 |aGeological Survey of Canada. |
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| 830 | #0|aOpen file (Geological Survey of Canada)|v3043|w(CaOODSP)9.506878 |
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| 856 | 40|qPDF|s2.38 MB|uhttps://publications.gc.ca/collections/collection_2018/rncan-nrcan/m183-2/M183-2-3043-eng.pdf |
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