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GEOPHYSICS DIVISION GEOLOGICAL SURVEY OF CANADA 1 OBSERVATORY CRESCENT, OTTAWA, ONTARIO, K1A 0Y3 Canada
Abstract
On 4 January 1992 an mbLg 6.0 earthquake occurred in a relatively aseismic section of the Boothia-Ungava Seismic Zone near Franklin Lake in the eastern Northwest Territories and was the third large earthquake to have occurred in eastern Canada since 1988. We have determined the source properties of this earthquake by modeling both body and surface waves. The focal mechanism indicates a combination of thrust and strike-slip faulting on a northwest-striking plane, with the rupture initiating at a depth of 9 km. The P axis of this focal mechanism is consistent with those of nearby earthquakes and with the regional stress field, which is dominated by near-horizontal northeast compression. MS and mb are about one unit of magnitude less than mbLg, which may be a result of directivity. There is some evidence based on a shift in corner frequency with azimuth that the fault ruptured to the southeast. Maximum likelihood estimates of the recurrence rates for the seismic zone suggest that, although the earthquake was unusually large for the immediate epicentral area, it was not anomalous with respect to the seismic zone as a whole. A comparative analysis of the mainshock and aftershocks indicates that the aftershocks tended to be shallower than the mainshock and probably had a larger component of dip-slip motion.
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