western quebec and southern ontario - Department of Geology

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$Fayek & Kyser 2000 uraninite fractionations.pdf - Queen's University$

DateDip(1)Strike(1)Rake(1)Table 4.4: Focal mechanisms obtained in this study.Dip(2)Strike(2)Rake(2)Trend(P)55Plunge(P)Trend(T)Plunge(T)solution polarity polarityerror1 19931116 45 ±4 169 ±6 90 ±2 45 ±4 349 ±7 90 ±2 169 ±7 3 ±2 135 ±20 86 ±2 50.0 11.0 0.0 A2 19931225 40 ±4 136 ±14 90 ±0 50 ±3 316 ±14 90 ±0 46 ±14 5 ±3 226 ±14 85 ±3 40.0 8.0 0.0 B3 19941002 48 ±2 14 ±10 90 ±0 42 ±2 194 ±12 90 ±0 104 ±11 3 ±2 284 ±11 87 ±2 23.0 7.0 0.0 C78 ±9 296 ±3 -90 ±0 12 ±8 116 ±1 -90 ±0 206 ±2 57 ±9 26 ±1 33 ±8 20.0 7.0 0.0 C4 19950215 61 ±7 125 ±9 64 ±5 38 ±1 349 ±4 127 ±10 233 ±6 12 ±3 350 ±6 65 ±8 5.0 10.0 0.0 A5 19950603 50 ±15 100 ±15 69 ±12 44 ±5 311 ±15 113 ±20 205 ±20 3 ±10 305 ±30 73 ±15 22.0 7.0 0.0 B65 ±11 77 ±11 54 ±6 43 ±4 317 ±14 141 ±15 192 ±9 13 ±7 301 ±17 55 ±7 21.0 7.0 0.0 B6 19950616 70 ±7 352 ±6 44 ±8 49 ±1 243 ±15 152 ±12 114 ±7 12 ±3 217 ±4 45 ±13 12.0 10.0 0.0 C62 ±15 135 ±10 -56 ±10 43 ±4 259 ±0 -137 ±20 93 ±5 58 ±18 201 ±5 11 ±10 7.0 10.0 0.0 C7 19950912 54 ±5 259 ±5 85 ±1 36 ±7 87 ±6 97 ±2 353 ±4 9 ±6 148 ±20 80 ±5 39.0 8.0 0.0 B50 ±6 116 ±2 90 ±0 40 ±1 296 ±1 90 ±0 206 ±1 5 ±1 26 ±1 85 ±1 3.0 8.0 0.0 B8 19951010 45 ±5 134 ±20 76 ±4 47 ±5 333 ±12 104 ±3 54 ±10 1 ±4 318 ±35 80 ±3 48.0 7.0 0.0 A9 19960314 69 ±7 96 ±14 60 ±7 36 ±0 334 ±7 143 ±15 208 ±10 18 ±5 327 ±10 55 ±10 25.0 9.0 0.0 B71 ±3 249 ±5 -58 ±2 36 ±2 7 ±3 -147 ±6 198 ±7 53 ±3 316 ±5 20 ±3 25.0 9.0 0.0 B10 19970403 9±4 78 ±20 -63 ±20 82 ±5 231 ±10 -94 ±3 137 ±10 53 ±4 325 ±10 37 ±4 30.0 11.0 0.0 C82 ±3 232 ±4 -90 ±0 8 ±3 52 ±5 -90 ±0 142 ±4 53 ±3 322 ±4 37 ±3 11.0 11.0 0.0 C11 19970524 36 ±0 116 ±13 83 ±14 54 ±14 305 ±8 95 ±4 31 ±6 9 ±20 236 ±25 80 ±18 49.0 17.0 0.0 C6 ±0 89 ±0 89 ±0 84 ±0 270 ±0 90 ±0 360 ±0 39 ±0 180 ±0 51 ±0 1.0 17.0 0.0 C12 19980226 42 ±4 309 ±13 53 ±10 57 ±5 174 ±15 119 ±7 244 ±15 8 ±4 137 ±7 64 ±5 46.0 13.0 1.0 B13 19980418 80 ±5 275 ±3 74 ±6 19 ±6 155 ±15 149 ±15 19 ±7 33 ±4 166 ±8 52 ±5 50.0 10.0 0.0 A14 19980730 34 ±2 174 ±6 90 ±0 56 ±3 354 ±10 90 ±0 84 ±9 11 ±3 264 ±8 79 ±3 25.0 13.0 0.0 C10 ±2 114 ±4 90 ±0 80 ±5 294 ±4 90 ±0 24 ±4 35 ±5 204 ±4 55 ±5 18.0 13.0 0.0 C15 19980925 46 ±1 356 ±3 53 ±1 55 ±1 224 ±3 122 ±1 292 ±3 4 ±2 193 ±6 64 ±0 8.0 8.0 0.0 C40 ±1 305 ±11 -109 ±7 53 ±1 149 ±5 -75 ±9 107 ±7 70 ±5 221 ±4 9 ±1 8.0 7.0 0.0 C16 19981225 42 ±0 328 ±0 24 ±0 74 ±0 221 ±0 130 ±0 282 ±0 19 ±0 171 ±0 46 ±0 1.0 11.0 0.0 A17 19990618 34 ±10 178 ±6 90 ±0 56 ±6 358 ±10 90 ±0 88 ±10 11 ±3 268 ±10 79 ±3 31.0 10.0 0.0 B10 ±4 114 ±4 90 ±0 80 ±5 294 ±4 90 ±0 24 ±4 35 ±5 204 ±4 55 ±5 19.0 10.0 0.0 B18 19991126 72 ±11 2 ±2 90 ±0 18 ±11 182 ±2 90 ±0 92 ±2 27 ±11 272 ±2 63 ±11 33.0 11.0 0.0 B19 20000101 56 ±9 126 ±3 90 ±0 34 ±9 306 ±3 90 ±0 216 ±3 11 ±9 36 ±3 79 ±9 31.0 15.0 0.0 B20 20000420 49 ±1 270 ±3 51 ±2 54 ±3 141 ±3 126 ±2 207 ±2 3 ±2 112 ±5 62 ±2 10.0 17.0 0.0 A21 20000806 55 ±2 308 ±5 73 ±5 38 ±1 156 ±5 113 ±7 50 ±3 9 ±2 171 ±6 73 ±4 6.0 17.0 0.0 AQuality
22 20001006 50 ±3 134 ±10 90 ±0 40 ±3 314 ±10 90 ±0 224 ±10 5 ±2 44 ±10 85 ±3 39.0 10.0 0.0 B23 20010126 43 ±5 259 ±20 -46 ±10 60 ±8 26 ±9 -123 ±2 246 ±20 60 ±7 139 ±12 10 ±7 25.0 9.0 0.0 D24 20010319 34 ±10 4 ±3 90 ±0 56 ±10 184 ±3 90 ±0 274 ±3 11 ±10 94 ±3 79 ±10 34.0 8.0 1.0 B25 20010411 59 ±10 4 ±12 90 ±0 31 ±10 184 ±8 90 ±0 95 ±3 14 ±10 273 ±10 76 ±10 50.0 12.0 1.0 B26 20011224 65 ±11 279 ±11 54 ±7 43 ±5 159 ±5 141 ±17 34 ±8 13 ±9 143 ±2 55 ±10 21.0 10.0 0.0 B55 ±2 122 ±8 73 ±6 38 ±1 330 ±3 113 ±9 224 ±5 9 ±1 345 ±11 73 ±5 20.0 10.0 0.0 B27 20020211 46 ±7 273 ±18 59 ±14 52 ±2 137 ±4 118 ±10 207 ±10 3 ±3 110 ±11 68 ±8 46.0 16.0 0.0 B28 20020420) 28 ±7 10 ±5 86 ±3 62 ±7 195 ±5 92 ±10 283 ±6 17 ±5 110 ±6 73 ±6 27.0 22.0 0.0 B6 ±1 36 ±8 90 ±0 84 ±4 216 ±8 90 ±0 306 ±8 39 ±4 126 ±8 51 ±4 24.0 22.0 0.0 B29 20020420 38 ±1 188 ±7 80 ±10 52 ±2 21 ±13 98 ±7 105 ±9 7 ±1 326 ±27 81 ±3 21.0 19.0 1.0 A30 20020907 43 ±3 173 ±5 75 ±12 49 ±5 13 ±10 103 ±4 93 ±6 3 ±3 347 ±15 80 ±8 20.0 9.0 0.0 B31 20030408 86 ±5 127 ±3 82 ±3 9 ±4 11 ±25 154 ±30 225 ±7 40 ±5 29 ±6 48 ±5 50.0 12.0 0.0 B27 ±4 312 ±1 76 ±5 64 ±5 147 ±6 97 ±2 232 ±5 19 ±5 71 ±7 70 ±4 50.0 12.0 0.0 B32 20030630 39 ±0 302 ±0 12 ±0 82 ±0 202 ±0 128 ±0 263 ±0 27 ±0 147 ±0 40 ±0 1.0 16.0 0.0 A33 20030820 79 ±5 257 ±3 51 ±2 40 ±1 154 ±7 163 ±7 16 ±2 24 ±4 130 ±3 42 ±1 9.0 13.0 0.0 A34 20031012 35 ±3 302 ±2 57 ±2 62 ±3 160 ±3 111 ±3 235 ±1 14 ±3 109 ±8 67 ±1 8.0 26.0 1.0 A35 20040804 65 ±3 298 ±2 -18 ±4 74 ±6 36 ±3 -154 ±3 259 ±2 29 ±3 166 ±3 5 ±6 26.0 24.0 0.0 B77 ±3 137 ±2 -25 ±2 65 ±3 233 ±2 -166 ±3 93 ±3 27 ±2 187 ±2 8 ±2 25.0 24.0 0.0 B36 20050303 68 ±11 140 ±4 90 ±0 22 ±11 320 ±4 90 ±0 230 ±4 23 ±11 50 ±4 67 ±11 35.0 11.0 0.0 B37 20050525 24 ±15 138 ±3 90 ±0 66 ±14 318 ±4 90 ±0 48 ±4 21 ±18 228 ±4 69 ±12 46.0 13.0 0.0 B38 20050704 50 ±0 289 ±3 80 ±1 40 ±1 125 ±1 102 ±2 27 ±1 5 ±0 148 ±4 81 ±1 3.0 18.0 0.0 A39 20050723 40 ±2 103 ±7 58 ±10 56 ±4 322 ±10 114 ±8 35 ±10 8 ±2 283 ±10 68 ±7 50.0 9.0 0.0 A40 20050906 38 ±0 134 ±0 80 ±0 52 ±0 327 ±0 98 ±0 52 ±0 7 ±0 272 ±0 81 ±0 1.0 12.0 0.0 A41 20051020 40 ±3 291 ±16 39 ±9 66 ±6 169 ±12 123 ±2 235 ±11 14 ±5 123 ±16 56 ±5 50.0 19.0 1.0 A42 20060109 40 ±0 290 ±0 87 ±3 50 ±0 114 ±3 93 ±2 202 ±2 5 ±0 44 ±10 85 ±1 3.0 15.0 2.0 A43 20060225 54 ±1 126 ±0 70 ±0 41 ±0 337 ±0 115 ±0 230 ±2 7 ±0 342 ±3 72 ±4 2.0 28.0 2.0 A44 20060620 49 ±6 243 ±10 -51 ±5 54 ±7 13 ±12 -126 ±6 222 ±20 62 ±2 127 ±7 3 ±5 50.0 20.0 2.0 A45 20070312 56 ±8 233 ±5 -80 ±1 35 ±8 36 ±1 -104 ±1 174 ±14 76 ±6 316 ±1 11 ±8 30.0 8.0 0.0 D46 20070930 30 ±8 126 ±7 90 ±0 60 ±8 306 ±8 90 ±0 36 ± 7 15 ±9 216 ±8 75 ±7 50.0 11.0 0.0 A47 20071001 47 ±1 131 ±3 47 ±5 58 ±2 5 ±3 126 ±2 70 ±3 6 ±3 330 ±3 59 ±4 16.0 13.0 0.0 A48 20071223 38 ±3 248 ±9 70 ±9 55 ±3 93 ±6 105 ±7 172 ±5 9 ±3 47 ±15 75 ±5 50.0 16.0 1.0 A49 20080109 48 ±10 336 ±15 44 ±10 58 ±10 212 ±15 128 ±5 276 ±8 6 ±8 177 ±18 57 ±2 47.0 9.0 0.0 C39 ±0 281 ±4 -71 ±13 53 ±5 77 ±15 -105 ±8 296 ±13 76 ±7 177 ±5 7 ±4 15.0 9.0 0.0 C50 20100623 65 ±4 132 ±5 59 ±6 39 ±2 7 ±8 139 ±12 244 ±3 15 ±3 359 ±4 58 ±7 24.0 47.0 2.0 A56
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 and 38: Fig. 3.1: Locations of seismic stat
Page 39 and 40: Figure 3.2: Number of stations used
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: some spatial variability of the ori
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
Page 89 and 90: a) b)c) d)Figure 5.9: Summary of th
Page 91 and 92: 5.4.3 Adirondack Clusters (WQ4 and
Page 93 and 94: WQ5 is located in the southern part
Page 95 and 96: Figure 5.13: Geological features of
Page 97 and 98: consistent with regional fault map
Page 99 and 100: WQ8 is locatedin the north-western
Page 101 and 102: 5.4.5 Timiskaming Cluster (WQ9)The
Page 103 and 104: The known faults in WQ9 cluster are
Page 105 and 106: a) b)c) d)Figure 5.19: Summary of t
Page 107 and 108: ecorded within this cluster. As it
Page 109 and 110: Figure 5.22: Nodal plane strike for
Page 111 and 112: estricted to western Lake Ontario o
Page 113 and 114: More detailed look at the relations
Page 115 and 116: Baird, W.A. F., and McKinnon, S. D.
Page 117 and 118:
Easton, R. M. (1986). Geochronology
Page 119 and 120:
Havskov, J., and Ottemöller, L. (2
Page 121 and 122:
Ma, S., and Adams, J. (2002). Estim
Page 123 and 124:
Rimando, R. E., and Benn, K. (2005)
Page 125 and 126:
Wahlstrom, R. (1987) Focal mechanis
Page 127 and 128:
APPENDIX A: Examples of Input and O
Page 129 and 130:
SUNO BZ SN 3 141 15.29SADO BZ SG 4
Page 131 and 132:
EEO BZ SG 4 140 48.02 91 0.09 0 315
Page 133 and 134:
PAL BZ PN 2 D 140 33.20 53 -0.21 1
Page 135 and 136:
APPENDIX C: Faults Plane Solutions
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128
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130
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134
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140
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142
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150
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Page 171 and 172:
Appendix D: Focal Mechanisms From P
Page 173 and 174:
19810707 -74.6 45.1 13.0 1.9 304.0
Page 175 and 176:
19950603 -76.4 47.1 18.0 3.9 100.1
Page 177 and 178:
20060225 -75.2 45.7 18.7 4.5 125.8
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168
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170
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