− | The knowledge required for working with seismic data is built of several layers like an onion. The figure below illustrates the idea. At the heart of the onion are 1-D seismic concepts like wavelet, convolution, traveltime, and reflection coefficient. All this shows up in the next layer, 2-D seismic, plus arrays, offset, dip, and lateral velocity variation. The next layer, 3-D seismic, includes all of 2-D plus azimuth, bins, and the data volume. Finally, 4-D seismic is time-lapse 3-D, which introduces repeatability, fluid flow, and difference volume.
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− | [[file:interpreting-seismic-data_fig12-1.png|thumb|{{figure number|12-1}}. Copyright: Liner, 1999; courtesy PennWell.]] | + | [[file:interpreting-seismic-data_fig12-1.png|thumb|{{figure number|1}}. Copyright: Liner, 1999; courtesy PennWell.]] |
| + | The knowledge required for working with seismic data is built of several layers like an onion. [[:file:interpreting-seismic-data_fig12-1.png|Figure 1]] illustrates the idea. At the heart of the onion are 1-D seismic concepts like wavelet, convolution, traveltime, and reflection coefficient. All this shows up in the next layer, 2-D seismic, plus arrays, offset, dip, and lateral velocity variation. The next layer, 3-D seismic, includes all of 2-D plus azimuth, bins, and the data volume. Finally, 4-D seismic is time-lapse 3-D, which introduces repeatability, fluid flow, and difference volume. |