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sgr ms thesis - University of Maine

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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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