Add to ORKGSingle-scattering imaging consists of two steps: wavefield extrapolation, whose goal is to reconstruct source and receiver wavefields from recorded data, and an imaging, whose goal is to extract from the extrapolated wavefields the locations where reflector
For various wavefield types, one can formulate a measurement of the mechanical energy that satisfies...
FIG. 4. Images obtained by applying the 2-D analog of equation (11) to synthetic data representing c...
Blended source and/or simultaneous source acquisition for multi-offset and multi-azimuth VSP measure...
Imaging under the single-scattering approximation consists of two steps: wave-field reconstruction o...
Common-angle wave-equation migration using the double-square-root is generally less accurate than th...
Conventional imaging algorithms assume single scattering and therefore cannot image multiply scatter...
10.1190/1.3223678scheme with little additional computational cost. Numerical tests on both synthetic...
Seismic imaging based on single-scattering approximation is in the analysis of the match between th...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
In areas of complex geology, migration-velocity estimation should use methods that describe the comp...
Correctly propagating waves from overhanging reflectors is crucial for imaging in complex geology. T...
Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Conselho Nacional de Desenvolvimento Ci...
Seismic imaging aims at revealing the structural information of the subsurface using the reflected w...
Wave-equation migration methods can more accurately account for complex wave phenomena than ray-trac...
Seismic imaging based on single-scattering approximation is based on analysis of the match between t...
For various wavefield types, one can formulate a measurement of the mechanical energy that satisfies...
FIG. 4. Images obtained by applying the 2-D analog of equation (11) to synthetic data representing c...
Blended source and/or simultaneous source acquisition for multi-offset and multi-azimuth VSP measure...
Imaging under the single-scattering approximation consists of two steps: wave-field reconstruction o...
Common-angle wave-equation migration using the double-square-root is generally less accurate than th...
Conventional imaging algorithms assume single scattering and therefore cannot image multiply scatter...
10.1190/1.3223678scheme with little additional computational cost. Numerical tests on both synthetic...
Seismic imaging based on single-scattering approximation is in the analysis of the match between th...
Standard imaging techniques rely on the single scattering assumption. This requires that the recorde...
In areas of complex geology, migration-velocity estimation should use methods that describe the comp...
Correctly propagating waves from overhanging reflectors is crucial for imaging in complex geology. T...
Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Conselho Nacional de Desenvolvimento Ci...
Seismic imaging aims at revealing the structural information of the subsurface using the reflected w...
Wave-equation migration methods can more accurately account for complex wave phenomena than ray-trac...
Seismic imaging based on single-scattering approximation is based on analysis of the match between t...
For various wavefield types, one can formulate a measurement of the mechanical energy that satisfies...
FIG. 4. Images obtained by applying the 2-D analog of equation (11) to synthetic data representing c...
Blended source and/or simultaneous source acquisition for multi-offset and multi-azimuth VSP measure...