KAUST DepartmentEarth Science and Engineering Program
Physical Sciences and Engineering (PSE) Division
KAUST Grant NumberOCRF-2014-CRG3-2300
Permanent link to this recordhttp://hdl.handle.net/10754/625974
MetadataShow full item record
AbstractTo decrease the recording time of a 2D seismic survey from a few days to one hour or less, we present a parsimonious surface-wave interferometry method. Interferometry allows for the creation of a large number of virtual shot gathers from just two reciprocal shot gathers by crosscoherence of trace pairs, where the virtual surface waves can be inverted for the S-wave velocity model by wave-equation dispersion inversion (WD). Synthetic and field data tests suggest that parsimonious wave-equation dispersion inversion (PWD) gives S-velocity tomograms that are comparable to those obtained from a full survey with a shot at each receiver. The limitation of PWD is that the virtual data lose some information so that the resolution of the S-velocity tomogram can be modestly lower than that of the S-velocity tomogram inverted from a conventional survey.
CitationLi J, Hanafy S, Schuster GT (2017) Parsimonious Surface Wave Interferometry. Geophysical Journal International. Available: http://dx.doi.org/10.1093/gji/ggx467.
SponsorsWe thank the sponsors for supporting the Consortium of Subsurface Imaging and Fluid Modeling (CSIM). We also thank KAUST for providing funding by the CRG grant OCRF-2014-CRG3-2300. For computer time, this research used the resources of the IT Research Computing Group and the Supercomputing Laboratory at KAUST.
PublisherOxford University Press (OUP)