title of the thesis - Department of Geology - Queen's University

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

P-axis B-axis T-axis Fault Plane 1 Fault Plane 2 Event Date Time Level Northing Easting Depth Trend Plunge Trend Plunge Trend Plunge Strike Dip Strike Dip fit% # 158 26/04/2006 11:03:58 7400 6300 4839 7358 61.0 51.0 258.0 37.0 161.0 8.0 100.0 63.0 216.0 49.0 71 159 24/04/2006 15:06:09 7400 6317 4871 7455 300.0 9.0 203.0 39.0 41.0 50.0 180.0 65.0 67.0 49.0 71 160 22/04/2006 11:50:29 7400 6453 4883 7450 150.0 50.0 28.0 24.0 284.0 30.0 213.0 79.0 326.0 27.0 88 161 21/04/2006 6:39:42 7400 6254 4465 7431 70.0 3.0 172.0 75.0 339.0 15.0 24.0 82.0 116.0 77.0 75 162 21/04/2006 2:35:13 7400 6239 4498 7420 267.0 84.0 122.0 5.0 31.0 4.0 306.0 49.0 116.0 42.0 86 163 15/04/2006 23:35:34 7400 6161 4340 7418 221.0 6.0 328.0 70.0 129.0 19.0 173.0 81.0 266.0 72.0 72 164 13/04/2006 21:12:21 7400 6331 4344 7376 336.0 3.0 234.0 64.0 69.0 26.0 205.0 77.0 109.0 68.0 65 165 12/04/2006 3:25:13 7400 6231 4659 7327 250.0 75.0 113.0 11.0 22.0 10.0 99.0 37.0 301.0 56.0 74 166 07/04/2006 13:59:30 7400 6278 4466 7456 208.0 67.0 57.0 20.0 323.0 10.0 250.0 58.0 30.0 39.0 67 167 04/04/2006 8:58:05 7400 6181 4386 7310 243.0 29.0 140.0 21.0 20.0 53.0 135.0 77.0 17.0 25.0 79 168 03/04/2006 17:49:39 7400 6168 4316 7373 183.0 11.0 279.0 29.0 74.0 59.0 116.0 62.0 242.0 42.0 84 169 03/04/2006 2:43:25 7400 6328 4789 7437 99.0 74.0 298.0 15.0 206.0 5.0 280.0 42.0 130.0 52.0 79 170 02/04/2006 7:49:10 7400 6118 4331 7338 227.0 54.0 107.0 20.0 5.0 28.0 292.0 76.0 54.0 25.0 73 171 30/05/2006 7:02:55 7400 6172 4318 7353 239.0 18.0 335.0 16.0 103.0 65.0 162.0 65.0 305.0 30.0 75 172 27/05/2006 17:22:40 7400 6162 4347 7393 312.0 27.0 201.0 36.0 70.0 43.0 194.0 81.0 92.0 37.0 77 173 15/05/2006 13:45:16 7400 6108 4374 7306 265.0 32.0 97.0 57.0 359.0 5.0 47.0 64.0 308.0 72.0 65 174 06/05/2006 13:51:29 7400 6228 4340 7426 204.0 27.0 94.0 34.0 324.0 44.0 88.0 81.0 344.0 35.0 71 175 30/05/2006 7:02:55 7400 6172 4318 7353 237.0 15.0 332.0 17.0 108.0 67.0 161.0 62.0 304.0 34.0 75 176 27/05/2006 17:22:40 7400 6162 4347 7393 313.0 28.0 201.0 35.0 71.0 42.0 195.0 82.0 94.0 37.0 77 177 23/05/2006 6:39:08 7400 6304 4887 7379 263.0 32.0 124.0 51.0 7.0 21.0 313.0 83.0 49.0 51.0 76 178 09/05/2006 5:38:27 7400 6294 4759 7417 282.0 6.0 39.0 77.0 191.0 11.0 327.0 78.0 236.0 86.0 74 179 09/05/2006 4:02:01 7400 6264 4710 7438 38.0 75.0 243.0 14.0 152.0 6.0 227.0 41.0 74.0 53.0 80 180 09/05/2006 3:48:22 7400 6286 4693 7459 103.0 42.0 245.0 41.0 354.0 20.0 233.0 77.0 129.0 44.0 81 181 05/05/2006 2:44:00 7400 6310 4880 7438 221.0 4.0 116.0 76.0 312.0 14.0 87.0 83.0 355.0 78.0 79 182 03/05/2006 8:25:31 7400 6170 4609 7315 291.0 20.0 121.0 70.0 22.0 3.0 335.0 79.0 68.0 74.0 74 183 30/06/2006 23:49:53 7400 6242 4764 7297 264.0 29.0 138.0 46.0 12.0 30.0 138.0 90.0 48.0 46.0 63 184 27/06/2006 7:41:46 7400 6291 4319 7451 165.0 3.0 258.0 46.0 73.0 44.0 110.0 63.0 219.0 59.0 83 160
P-axis B-axis T-axis Fault Plane 1 Fault Plane 2 Event # Date Time Level Northing Easting Depth Trend Plunge Trend Plunge Trend Plunge Strike Dip Strike Dip fit% 185 26/06/2006 4:16:07 7400 6257 4795 7378 220.0 73.0 74.0 14.0 342.0 9.0 55.0 38.0 264.0 56.0 74 186 25/06/2006 10:19:17 7400 6066 4692 7379 197.0 45.0 96.0 11.0 355.0 43.0 276.0 89.0 10.0 11.0 82 187 24/06/2006 18:56:57 7400 6159 4359 7367 357.0 28.0 106.0 32.0 235.0 45.0 292.0 80.0 38.0 34.0 77 188 24/06/2006 0:53:35 7400 6349 4758 7438 43.0 64.0 159.0 12.0 254.0 23.0 154.0 69.0 7.0 25.0 84 189 23/06/2006 17:24:50 7400 6188 4745 7362 213.0 70.0 303.0 0.0 34.0 20.0 303.0 65.0 124.0 25.0 82 190 23/06/2006 5:34:19 7400 6342 4752 7442 47.0 86.0 199.0 4.0 290 2.0 23.0 43.0 196.0 47.0 67 191 22/06/2006 14:44:03 7400 6205 4482 7307 140.0 12.0 246.0 52.0 41.0 35.0 86.0 75.0 187.0 56.0 83 192 21/06/2006 15:54:34 7400 6186 4539 7389 318.0 23.0 193.0 54.0 60.0 26.0 190.0 88.0 98.0 54.0 80 193 20/06/2006 4:47:23 7400 6367 4456 7496 92.0 2.0 182.0 64.0 1.0 26.0 44.0 74.0 140.0 71.0 68 194 06/06/2006 4:02:43 7400 6130 4374 7437 50.0 21.0 176.0 57.0 310.0 24.0 360.0 88.0 91.0 58.0 69 195 09/06/2006 16:31:39 7400 6202 4660 7352 87.0 44.0 264.0 46.0 355.0 1.0 122.0 60.0 230.0 62.0 89 196 15/06/2006 19:07:06 7400 6150 4355 7368 17.0 6.0 282.0 38.0 115.0 51.0 257.0 61.0 141.0 51.0 67 197 13/06/2006 3:27:21 7400 6087 4953 7375 18.0 25.0 208.0 64.0 109.0 4.0 61.0 75.0 156.0 69.0 69 161
Page 1 and 2:
THE INFLUENCES OF STRESS AND STRUCT
Page 3 and 4:
esulting in increased stress to the
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Table of Contents Abstract.........
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4.6.1 Fracture Reactivation........
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List of Figures Figure 1.1: Locatio
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Figure 3.23: Preliminary stress inv
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Figure B11: Events between Jan 1, 2
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List of Tables Table 2.1: Geologica
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Chapter 1 Introduction 1.1 Backgrou
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Figure 1.1: Location of Sudbury and
Page 21 and 22:
Chapter 2 Geological Assessment of
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ack breccia and sediments later dep
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Murray Fault, the principal fault o
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2.2 Local Geology of Creighton Mine
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B West East B’ Figure 2.4B: Longi
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Table 2.2: Fault systems within the
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Table 2.3: Summary of Fault Charact
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Figure 2.6: (A) Damage to shotcrete
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Figure 2.7: (A) The 1290 Shear Zone
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Figure 2.8: Images of (A) the 400-E
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Figure 2.9: (A) Photograph of the c
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Figure 2.10 (A) Shear foliation, in
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Figure 2.11: Thin sections of the F
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(Fig. 2.12B). Reduction of quartz g
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2.3.11 Late-Stage Fractures The you
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overprinting (Cochrane, 1991; Couls
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Table 2.4: Summary of Proterozoic t
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Both of these inferred stress direc
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are, at this time, in the process o
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Microseismic events of this subset
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3.2.1.2 Seismic Energy (E o ) and S
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3.2.1.4 Stress Parameters Stress pa
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located events were removed from cl
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Figure 3.7: Detected seismicity cor
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Table 3.1: Event characteristics in
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Table 3.3: Summary of relevant para
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) Damage Zone The rock mass in the
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quadrants of dilatation and compres
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Figure 3.12: Lower hemisphere equal
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mechanism shows that over 57% of th
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Figure 3.16: Classification of prin
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Figure 3.18: Contoured P-axis, B-ax
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Figure 3.20: Distribution of double
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This parameter reflects the magnitu
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Figure 3.23: Preliminary stress inv
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Figure 3.25: Equal area stereonet s
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Figure 3.27: (A) Maximum principal
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4.2 Numerical Methods Phase 2 and U
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Stress-strain relationships are use
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Rock mass failure is governed by th
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Figure 4.5: (A) Model for tectonic
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The zero cohesion and low friction
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Figure 4.9: Model of yielding for C
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Figure 4.11: Model of differential
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Figure 4.14: Model of maximum stres
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stress field model. There is little
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clustering are indications of rock
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Figure 4.23: Contoured domains of s
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Figure 4.24: Fracture initiation th
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seismic Cluster 1, which correspond
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contains energetic events and is no
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preferentially oriented fracture pl
Page 125 and 126: methodologies employed are of value
Page 127 and 128: References Alcott, J. M., Kaiser, P
Page 129 and 130: Galkin, V., Mungall, J. (2005). Str
Page 131 and 132: Mungall, J. E., & Hanley, J. J. (20
Page 133 and 134: Appendix A Geological Maps and Samp
Page 135 and 136: A.2 Level Plans with Sample Locatio
Page 137 and 138: Figure A3: 7400 Level, modified for
Page 139 and 140: Figure A5: 7680 Level, modified for
Page 141 and 142: Figure A7: 7940 Ramp, modified from
Page 143 and 144: MICROSEISMIC EVENTS Source Radius A
Page 145 and 146: 2006 Event Frequency with Depth 600
Page 147 and 148: B.2 Spatial Distribution of Seismic
Page 149 and 150: Figure B11: Events between Jan 1, 2
Page 155 and 156: Cluster 1 Source Radius Asp. Radius
Page 157 and 158: Seismic Moment 10.0 9.5 9.0 8.5 8.0
Page 159 and 160: 143 Peak Velocity Parameter -2.5 -2
Page 161 and 162: B.4.2 Temporal Distribution of Clus
Page 163 and 164: 147 Static Stress Drop 5.0 5.5 6.0
Page 165 and 166: B.4.3 Temporal Distribution of Clus
Page 167 and 168: 151 Static Stress Drop 4.0 4.5 5.0
Page 169 and 170: Frequency-Magnitude Relation for Cl
Page 171 and 172: P-axis B-axis T-axis 155 Fault Plan
Page 173 and 174: P-axis B-axis T-axis Fault Plane 1
Page 175: P-axis B-axis T-axis Fault Plane 1
Page 179 and 180: D.1.1: Case 1 Models Figure D1: Cas
Page 181 and 182: Figure D3: Case 1, elastic models s
Page 183 and 184: A B C D Figure D5: Case 1, plastic
Page 185 and 186: A B C D Figure D7: Case 1, plastic
Page 187 and 188: D.1.2: Case 2 Models A B C D Figure
Page 189 and 190: D.1.3: Case 3 Models A B C Figure D
Page 191 and 192: D1.4 Tectonic Loading Models Figure
Page 193 and 194: D.2 Discussion of Phase 2 Models El
Page 195 and 196: Staged models were created in which
Page 197 and 198: Figure D17 (A) Elastic model showin
Page 199 and 200: Figure D19 (A) Elastic model showin
Page 201 and 202: • Similar damage zones surroundin
Page 203 and 204: ; ;================================
Page 205 and 206: change jmat=1 range 0,1564.64 0,156
Page 207 and 208: crack (845.579,718.676) (787.063,57
Page 209 and 210: ;===plum=== crack (0,355.2371429) (
Page 211 and 212: crack (866.14,726.44) (838.2,737.61
Page 213 and 214: crack (838.2,737.616) (815.848,771.
Page 215 and 216: crack (815.848,771.144) (815.848,78
Page 217 and 218: ;===== define sub block ===========
Page 219 and 220: E.9 S3:S1 Model for fracture reacti
Page 221 and 222: yval= abs(z_syy(zi)) xyval= abs(z_s
Page 223 and 224: and rearranged to , (Equation F4) .
Page 225: Such that , (Equation F19) I is the
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title of the thesis - Department of Geology - Queen's University

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