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

Early to Middle Jurassic Salt in Baltimore Canyon Trough

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Figure 3B. True-amplitude-processed sections of profiles shown in Figure 2. These exemplify the anomalously high amplitude of the negative-polarity reflector. Vertical scale is two-way traveltime.

Figure 3. True-amplitude-processed sections of profiles shown in Figure 2.

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