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- W2010097079 abstract "Frequency variations are due in part to different specifications of the instruments and in part to the different coupling characteristics of the media involved-water, mud, and dry sediment, We expect a different frequency response from a 10 Hz resonant detector in water than from an 8 Hz resonant detector in dry sand, And, in fact, after phase compensation, we see a smoother, broader frequency spectrum in the water-covered zones compared to the land or marsh zones. An estimated signature for each detector type indicates the bandwidth passed by the different instruments. Selecting and applying a cotimon bandwidth to the data set eliminates the frequency variation along the line." @default.
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- W2010097079 date "1982-01-01" @default.
- W2010097079 modified "2023-09-25" @default.
- W2010097079 title "Binning and Time‐Variant Regridding of 3‐D Seismic Data" @default.
- W2010097079 doi "https://doi.org/10.1190/1.1807564" @default.
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