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

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2.5.1.2 Descriptions <strong>of</strong> quartz CPO patterns ...................................................................... 38<br />

2.5.1.3 Quartz CPO deformation temperatures .................................................................. 45<br />

2.5.2 Rigid clast vorticity analysis ......................................................................................... 47<br />

2.5.3 Summary <strong>of</strong> microstructural analyses ........................................................................... 50<br />

2.6 Geochronology and <strong>the</strong>rmochronology ............................................................................... 52<br />

2.6.1 U-Th-Pb monazite geochronology ................................................................................ 53<br />

2.6.1.1 Methodology .......................................................................................................... 54<br />

2.6.1.2 Results .................................................................................................................... 55<br />

2.6.1.3 Summary <strong>of</strong> U-Th-Pb geochronology .................................................................... 69<br />

2.6.2 40 Ar/ 39 Ar <strong>the</strong>rmochronology .......................................................................................... 71<br />

2.6.2.1 Methodology .......................................................................................................... 72<br />

2.6.2.2 Results .................................................................................................................... 74<br />

2.6.2.3 Summary <strong>of</strong> 40 Ar/ 39 Ar <strong>the</strong>rmochronology .............................................................. 79<br />

2.7 Discussion ............................................................................................................................ 81<br />

2.7.1 South-directed extrusion <strong>of</strong> <strong>the</strong> GHS ............................................................................ 83<br />

2.7.1.1 Initial south-directed extrusion .............................................................................. 83<br />

2.7.1.2 Timing <strong>of</strong> south-directed extrusion ........................................................................ 84<br />

2.7.2 Orogen-parallel extension ............................................................................................. 85<br />

2.7.2.1 ESE-WNW deformation and exhumation .............................................................. 85<br />

2.7.2.2 Timing <strong>of</strong> ESE-WNW deformation and cooling ................................................... 87<br />

2.7.3 Transition from south-directed extrusion to orogen-parallel extension ........................ 88<br />

2.7.3.1 Upper Karnali valley .............................................................................................. 88<br />

2.7.3.2 Himalayan transition .............................................................................................. 90<br />

2.7.4 Tectonic model explaining orogen-parallel extension .................................................. 94<br />

2.8 Conclusions .......................................................................................................................... 97<br />

Chapter 3 Discussion ................................................................................................................... 99<br />

3.1 Summary .............................................................................................................................. 99<br />

3.1.1 Middle Miocene orogen-parallel extension and east-directed lower-crustal flow ........ 99<br />

3.2 Future research considerations ........................................................................................... 103<br />

3.2.1 Why did south-directed mid-crustal extrusion cease, and why did east-directed lower<br />

crustal flow initiate ............................................................................................................. 103<br />

3.2.2 Is <strong>the</strong> Karakoram fault linked to faults <strong>of</strong> <strong>the</strong> upper Karnali valley .......................... 104<br />

Chapter 4 Microstructural analyses: proposals for advancing and validating current<br />

techniques ................................................................................................................................... 106<br />

viii

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