Interpretation · 2015 · 17 citations · 4 references
Natural SciencesEarth SciencesGeophysicsDigital ImagingExploration GeophysicsSeismologySeismic Data AcquisitionSeismic Data ProcessingSeismic ExplorationSeismic ImagingSeismic ReflectionSubsurface ImagingOptimal RotationSeismic Imaging Of Subsurface StructuresSeismic Reflection ImagingSteeringSurface ProfileWave Ray Tracing
Abstract We have analyzed vertical seismic profile (VSP) data acquired across a Marcellus Shale prospect and found that SV-P reflections could be extracted from far-offset VSP data generated by a vertical-vibrator source using time-variant receiver rotations. Optimal receiver rotation angles were determined by a dynamic steering of geophones to the time-varying approach directions of upgoing SV-P reflections. These SV-P reflections were then imaged using a VSP common-depth-point transformation based on ray tracing. Comparisons of our SV-P image with P-P and P-SV images derived from the same offset VSP data found that for deep targets, SV-P data created an image that extended farther from the receiver well than P-P and P-SV images and that spanned a wider offset range than P-P and P-SV images do. A comparison of our VSP SV-P image with a surface-based P-SV profile that traversed the VSP well demonstrated that SV-P data were equivalent to P-SV data for characterizing geology and that a VSP-derived SV-P image could be used to calibrate surface-recorded SV-P data that were generated by P-wave sources.
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