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ACQUISITION/PROCESSING |
University of Houston, Texas, USA
Lawrence Berkeley National Laboratory, California, USA
University of California at Berkeley, USA
West-Siberian Research Institute of Geology and Geophysics, Tyumen, Russia
Corresponding author: ggoloshubin{at}uh.edu
Abstract
There are numerous laboratory and field examples in which low-frequency components of reflected seismic waves show surprising imaging capabilities. Ironically, such components are often filtered out as useless in conventional data processing. However, as we demonstrate below, this part of the signal contains the most important information about the reservoir.
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