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structural geology, propagation mechanics and - Stanford School of ...

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Normalized thickness<br />

1.4<br />

1.2<br />

1.0<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0.0<br />

-1.0 -0.5 0.0 0.5 1.0<br />

(a) Distance from center normalized by trace half-length<br />

Midpoint thickness (mm)<br />

(b)<br />

Thickness (mm)<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

0 5 10 15 20 25<br />

Trace half-length (m)<br />

30 35<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

(c)<br />

-1 -0.5 0 0.5<br />

Distance from center normalized by trace half-length<br />

1<br />

Figure 2.4. (a) Thickness pr<strong>of</strong>ile data for 16 tip-to-tip compaction b<strong>and</strong> traces (>1,700<br />

measurements). Position is normalized relative to center by the b<strong>and</strong> half length <strong>and</strong><br />

thickness is normalized by the midpoint value. The curved line represents an ellipse<br />

similarly normalized. The correlation index <strong>of</strong> the data to the ellipse is 0.79. (b) Plot <strong>of</strong><br />

midpoint thickness versus trace half-length for the 16 compaction b<strong>and</strong> pr<strong>of</strong>iles, star<br />

indicates CB shown in (c). Thickness generally increases with increasing length, but<br />

along a decreasing trend. (c) Thickness pr<strong>of</strong>ile for CB-A, the 24.75-m-long compaction<br />

b<strong>and</strong> trace featured in this paper. The curved line represents the least-squares best fit <strong>of</strong><br />

an ellipse to the data. The correlation index for this fit is 0.87.<br />

49

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