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Figure 6.4.<br />
Figure 6.5.<br />
Type 3 Shatter Zone .................................................................... 69<br />
Centimeter-scale boudinage textures in Bar Harbor<br />
Formation ..................................................................................... 70<br />
Figure 6.6.<br />
Figure 6.7.<br />
Figure 6.8.<br />
Brecciation textures in Type 2 Shatter Zone ................................ 72<br />
Local flow textures in Type 3 Shatter Zone .................................. 73<br />
Evidence for secondary clast size, shape, and boundary<br />
modification ................................................................................. 75<br />
Figure 6.9.<br />
Figure 6.10.<br />
Figure 6.11.<br />
Figure 6.12.<br />
Figure 6.13.<br />
Figure 7.1.<br />
Figure 7.2.<br />
Figure 7.3.<br />
Figure 7.4.<br />
Figure 7.5.<br />
An outcrop grid used for fractal analysis ...................................... 77<br />
Clast size distribution data for Type 1 and 2 Shatter Zone ........... 80<br />
Clast size distribution data for Type 3 Shatter Zone .................... 81<br />
Clast boundary shape data ordered by Shatter Zone type .......... 83<br />
Circularity data ordered by Shatter Zone type .............................. 85<br />
Geometries used for thermal modeling ........................................ 93<br />
Solidus migration trend for a spherical clast ............................... 100<br />
A plot displaying clast melt over time ......................................... 101<br />
Temperature changes over time for points in a clast ................. 103<br />
The evolution <strong>of</strong> clast size distribution with progressive<br />
thermal exposure ....................................................................... 107<br />
Figure 7.6.<br />
Figure 7.7.<br />
Clast geometry used for thermal stress analysis ........................ 111<br />
Time step results for thermal stress in metasedimentary and<br />
diorite clasts ............................................................................... 113<br />
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