27.10.2014 Views

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

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

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

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

List <strong>of</strong> Figures<br />

Figure 1.1: Location <strong>of</strong> Sudbury and Creighton Mine...................................................................3<br />

Figure 2.1: (A) Location map <strong>of</strong> Sudbury in Ontario, Canada (B); <strong>the</strong> location <strong>of</strong> <strong>the</strong><br />

Sudbury and surrounding tectonic provinces ............................................................5<br />

Figure 2.2: Local geology map. ...................................................................................................10<br />

Figure 2.3: Horizontal view <strong>of</strong> a fault jog in proximity to Creighton Fault.................................10<br />

Figure 2.4:Cross-section <strong>of</strong> Creighton Mine showing geometry <strong>of</strong> footwall and<br />

hangingwall rocks as well as orebodies....................................................................12<br />

Figure 2.5: Representative level plan for <strong>the</strong> Creighton Deep....................................................15<br />

Figure 2.6: Images <strong>of</strong> <strong>the</strong> Footwall Shear...................................................................................19<br />

Figure 2.7: (A) The 1290 Shear Zone fabric; (B) 1290 Shear Zone on <strong>the</strong> 6400 Level;<br />

and (C) biotite, quartz and calcite fabric <strong>of</strong> <strong>the</strong> 1290 shear zone. ............................21<br />

Figure 2.8: Images <strong>of</strong> <strong>the</strong> 400-East Shear Zone..........................................................................23<br />

Figure 2.9: (A) Photograph <strong>of</strong> <strong>the</strong> cracked concrete pad floor along <strong>the</strong> Return Air Raise<br />

Shear Zone on 7530L; (B) cracked shotcrete on wall <strong>of</strong> 7530L; (C) thin<br />

section <strong>of</strong> shear zone fabric on 7680L; (D) thin section <strong>of</strong> shear zone fabric<br />

on 7400 <strong>the</strong> Level.....................................................................................................25<br />

Figure 2.10: Reactivated structures in proximity to <strong>the</strong> Plum Shear Zone ..................................27<br />

Figure 2.11: Thin sections <strong>of</strong> <strong>the</strong> Fresh Air Raise Shear .............................................................29<br />

Figure 2.12: Images <strong>of</strong> <strong>the</strong> Fresh Air Raise-Type Shear..............................................................30<br />

Figure 2.13: Images <strong>of</strong> <strong>the</strong> Grizzly Splay. ...................................................................................32<br />

Figure 2.14: Shallow shear fractures in Creighton Deep. ............................................................33<br />

Figure 2.15: Block model depicting paleokinematics <strong>of</strong> mine-scale faults in <strong>the</strong> Creighton<br />

Deep .........................................................................................................................34<br />

Figure 2.16: Riedel Model <strong>of</strong> 1290 and 118-System shear zones................................................38<br />

Figure 2.17: NW-SE Penokean compression...............................................................................38<br />

Figure 3.1: Plan view <strong>of</strong> events related to development blasts production blast-induced<br />

events........................................................................................................................42<br />

Figure 3.2: Distribution <strong>of</strong> Microseismic Event Magnitudes between January 1, 2006 and<br />

December 31, 2007 recorded between 7000 and 7600 feet depth............................44<br />

ix

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!