ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Publication Date: 2014-07-02
    Description: On 10 October 2012 a moderate, Nuttli magnitude ( M N ) 4.5, earthquake occurred in the Montreal region. Although it did not cause any damage, it was felt throughout the region and at distances to a few hundred kilometers. The earthquake was very well recorded by seismographs at regional distances, allowing its source parameters (such as focal mechanism and depth) to be determined. Both the regional moment tensor inversion and first-motion methods indicate predominantly thrust faulting on a northwest-striking plane, which is typical of the west Quebec seismic zone. A depth of 13–15 km was indicated by the regional moment tensor inversion and by the regional depth phase method. The moment magnitude of 3.7 is slightly smaller than would be expected based on the average M N – M w relation but is well within the range of observed values for previous earthquakes. More than 10,000 felt reports were received via an Internet "Did You Feel It?" page. A few weeks later, on 6 November 2012, another moderate ( M N  4.2, M w  3.9) earthquake occurred in the west Quebec seismic zone but in a different location, near the Quebec–Ontario border. This event also had a northwest predominantly thrust mechanism. Depths obtained by regional moment tensor and depth phase methods were both in the 6–8 km range. Over 2500 online felt reports were received. The earthquakes provided a successful test of recent changes made to handle high volumes of Internet traffic that typically occur after a significant earthquake felt in a large, urban area.
    Print ISSN: 0895-0695
    Electronic ISSN: 1938-2057
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2015-03-05
    Description: Although moderate in size ( M N  5.2, M  4.6), the earthquake that occurred near Ladysmith, Quebec, on 17 May 2013 was one of the best-recorded earthquakes to have occurred in eastern Canada in recent years due to the fortuitous deployment of U.S. Transportable Array stations in a region that was already well covered by the Canadian National Seismograph Network. This data set allowed us to study the earthquake and its aftershocks in better detail than we could have done in the past. Moment tensor and first-motion focal mechanisms suggest that it was a typical western Quebec earthquake resulting from thrust faulting on a northwest-striking plane. Several methods were used to determine the depth, all indicating a depth of 12–15 km. The aftershock sequence, which included a magnitude 4.1 ( M N ) earthquake occurring 10 min after the mainshock, was relatively rich in M N 〉3.0 events and contrasts sharply with that of the 2010 Val-des-Bois earthquake (also in western Quebec). Strong-motion data from the Ladysmith earthquake contributed to an ongoing study to model soft soil amplification and basin effects. The earthquake was felt to distances in excess of 500 km, and more than 4300 people filled out an online "Did You Feel It?" survey, providing a detailed picture of macroseismic effects. Visits to Ladysmith and nearby communities found evidence for minor damage confined to the epicentral area. It is difficult to correlate the Ladysmith sequence with any known faults in the region, but it is noted that some local-scale lineaments in the epicentral area trend subparallel to the nodal planes of the focal mechanism.
    Print ISSN: 0895-0695
    Electronic ISSN: 1938-2057
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...