Enhancing Shallow Seismic Reflection Profiles Using Nonlinear Correlation: Applications to the New Jersey Margin.
LAMONT-DOHERTY EARTH OBSERVATORY PALISADES NY
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Some older Multichannel Seismic data recorded on the shallow continental shelf do not properly image the upper few 100 m. This is due to a large approx. 200 m minimum source receiver offset. Nonlinear Correlation, used successfully for other seismic processing was not able to correct the data. The use of a short Approx. 30 m minimum source receiver offset produces excellent seismic images of the upper sediments.
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