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| | Abstract | | A CRS operator is described by the three kinematic wavefield parameters (alpha, KN, and KNIP) and they are automatically analyzed from data at every zero-offset sample. Since CRS parameters can be converted to RMS velocity, a high-density RMS velocity field is obtained without much human intervention. This objectively-analyzed velocity is beneficial especially in geologically complex areas, as well as enhanced stack section derived by CRS/MDRS method. |
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