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U.S. Geological Survey Open-File Report 2004-1435

Early to Middle Jurassic Salt in Baltimore Canyon Trough

skip index. Title Page  /  Abstract  /  Introduction  /   Geologic Setting  /   Data Collection  /  Data Processing  /  Geophysical Analysis  /  Discussion  /  Conclusion  /   Bibliography  /  Figures  /  Tables


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Figure 5. Amplitude versus offset analysis for Line 10 near CMP 4250. Reflection coefficient versus incident angle is plotted for both positive and negative reflection coefficients. Solid lines show least-squares fit solution. Note that reflection coefficient decreases with increasing offset.

Figure 5. Amplitude versus offset analysis for Line 10 near CMP 4250.

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