- Page 1 and 2: FOCAL MECHANISMS AND VARIATIONS IN
- Page 3: Acknowledgements:I would like to ex
- Page 9 and 10: Figure 5.12: Summary of the focal m
- Page 11 and 12: AbbreviationsCNSN: Canadian Nationa
- Page 13 and 14: Earthquakes in western Quebec and s
- Page 15 and 16: 1.2 Organization of ThesisChapter 1
- Page 17 and 18: eastern Canada each year, of which
- Page 19 and 20: Metasedimentary Belt boundary tecto
- Page 21 and 22: The Grenville Front tectonic zone (
- Page 23 and 24: Figure 2.3: Seismicity in the study
- Page 25 and 26: oadly similar continent-continent c
- Page 27 and 28: Figure 2.4: Historical earthquakes
- Page 29 and 30: earthquakes have occurred within th
- Page 31 and 32: cluster, which is considered part o
- Page 33 and 34: 2001. All events seemed to occur in
- Page 35 and 36: CHAPTER 3DATA SET AND METHODS3.1 In
- Page 37: Fig. 3.1: Locations of seismic stat
- Page 41 and 42: the strongest recorded event in the
- Page 43 and 44: Figure 3.5: Earthquake source param
- Page 45 and 46: The amplitudes of the seismic waves
- Page 47 and 48: Figure 3.7: Vertical component wave
- Page 49 and 50: HYPOCENTER programThe HYPOCENTER pr
- Page 51 and 52: wave - e.g. Pg or Pn, Sg or Sn), th
- Page 53 and 54: model for P-wave velocity with mult
- Page 55 and 56: CHAPTER 4RESULTSIn this chapter the
- Page 57 and 58: Figure 4.1: Distribution of RMS of
- Page 59 and 60: Table 4.2: Earthquake parameters (h
- Page 61 and 62: The focal depth calculated here is
- Page 63 and 64: focal mechanism beach-ball diagrams
- Page 65 and 66: some spatial variability of the ori
- Page 67 and 68: 22 20001006 50 ±3 134 ±10 90 ±0
- Page 69 and 70: a)b)c)d)Western QuebecSouthern Onta
- Page 71 and 72: esults from other similar studies,
- Page 73 and 74: source region (e.g. Chen and Molnar
- Page 75 and 76: estimate using a stress inversion t
- Page 77 and 78: Figure 5.3: Stress pattern for all
- Page 79 and 80: oundaries of the Central Metasedime
- Page 81 and 82: In Western Quebec Seizmic Zone (WQS
- Page 83 and 84: deeper than 20 km (20 km to 26 km).
- Page 85 and 86: Figure 5.7: Geologic features of WQ
- Page 87 and 88: 2009). The Mont-Laurier earthquake
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a) b)c) d)Figure 5.9: Summary of th
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5.4.3 Adirondack Clusters (WQ4 and
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WQ5 is located in the southern part
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Figure 5.13: Geological features of
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consistent with regional fault map
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WQ8 is locatedin the north-western
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5.4.5 Timiskaming Cluster (WQ9)The
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The known faults in WQ9 cluster are
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a) b)c) d)Figure 5.19: Summary of t
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ecorded within this cluster. As it
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Figure 5.22: Nodal plane strike for
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estricted to western Lake Ontario o
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More detailed look at the relations
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Baird, W.A. F., and McKinnon, S. D.
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Easton, R. M. (1986). Geochronology
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Havskov, J., and Ottemöller, L. (2
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Ma, S., and Adams, J. (2002). Estim
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Rimando, R. E., and Benn, K. (2005)
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Wahlstrom, R. (1987) Focal mechanis
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APPENDIX A: Examples of Input and O
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SUNO BZ SN 3 141 15.29SADO BZ SG 4
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EEO BZ SG 4 140 48.02 91 0.09 0 315
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PAL BZ PN 2 D 140 33.20 53 -0.21 1
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APPENDIX C: Faults Plane Solutions
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Appendix D: Focal Mechanisms From P
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19810707 -74.6 45.1 13.0 1.9 304.0
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19950603 -76.4 47.1 18.0 3.9 100.1
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20060225 -75.2 45.7 18.7 4.5 125.8
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