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FRACTAL ANALYSIS AND THERMAL-ELASTI
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LIBRARY RIGHTS STATEMENT In present
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emplacement of mafic magma, resulti
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© 2011 Samuel Geoffrey Roy All Rig
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TABLE OF CONTENTS ACKNOWLEDGEMENTS
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5.3.5. Clast Circularity Analysis .
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LIST OF FIGURES Figure 2.1. Figure
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LIST OF TABLES Table 6.1. Table 7.1
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subvolcanic magmatic systems, the l
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Chapter 2 GEOLOGIC SETTING 2.1. Reg
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Somesville granite suite to the wes
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Biotite is metamorphic in origin, a
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Chapter 3 PHYSICAL DESCRIPTION OF S
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thinned lithosphere allows for part
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A B C Figure 3.1. Formation of a la
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1997; Branney and Kokelaar, 1998; J
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- Page 41 and 42: Chapter 4 THERMAL FRAMEWORK FOR CON
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- Page 45 and 46: A B Grt C Grt D Crd Crd E 1 mm F Cr
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- Page 49 and 50: 4.3.1. Model Setup The model is use
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- Page 53 and 54: t = 0s t = 1E11 t = 1E12s t = 1E13s
- Page 55 and 56: 850 750 650 550 450 400m Into Chamb
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- Page 59 and 60: Chapter 5 ROCK MECHANICS AND THE FR
- Page 61 and 62: A β δ σ 1 σ 3 σ t c a σ 1 σ
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- Page 65 and 66: h h/2 h/4 Figure 5.2. A cube displa
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- Page 79 and 80: Chapter 6 ANALYSIS AND RESULTS The
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- Page 87 and 88: A B Figure 6.6. Brecciation texture
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- Page 101 and 102: with decreasing clast size in all T
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- Page 107 and 108: magma. To prove the viability of th
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- Page 115 and 116: Dimensionless time 0 0.05 0.1 0.15
- Page 117 and 118: Figure 7.4 displays model results f
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- Page 131 and 132: disaggregation of Bar Harbor clasts
- Page 133 and 134: REFERENCES Acocella, V. (2007). Und
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Billen, M.I. and Gurnis, M. (2001).
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Clarke, D. B. (2007). Assimilation
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Fisher, R.V. (1960). Classification
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Hartmann, W.K. (1969). Terrestrial,
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Johnson, S.E.; Paterson, S.R.; Tate
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Mandelbrot, B.B. (1967). How long i
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Oliver, N.H.S.; Rubenach, M.J.; Fu,
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Schoutens, J.E. (1979). Empirical A
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Wiebe, R.; Holden, J.; Coombs, M.;