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Figure 1 – Chair display showing an incised channel on a coherence stratal slice and its seismic amplitude signature. We interpret the sag over the channel to indicate that it contains more shale than the surrounding matrix.
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Figure 1 – Chair display showing an incised channel on a coherence stratal slice and its seismic amplitude signature. We interpret the sag over the channel to indicate that it contains more shale than the surrounding matrix.