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Early detection of stress changes and failure using acoustic measurements
Early detection of stress changes and failure using acoustic measurements
Applying source-receiver Marchenko redatuming to field data, using an adaptive double-focusing method
Applying source-receiver Marchenko redatuming to field data, using an adaptive double-focusing method
Reflecting boundary conditions for interferometry by multidimensional deconvolution.
Reflecting boundary conditions for interferometry by multidimensional deconvolution.
Marchenko redatuming for multiple prediction and removal in situations with a complex overburden
Marchenko redatuming for multiple prediction and removal in situations with a complex overburden
Deep ocean sound speed characteristics passively derived from the ambient acoustic noise field
Deep ocean sound speed characteristics passively derived from the ambient acoustic noise field
Application of seismic interferometry by multidimensional deconvolution to ambient seismic noise recorded in Malargüe, Argentina
Application of seismic interferometry by multidimensional deconvolution to ambient seismic noise recorded in Malargüe, Argentina
Imaging an unknown object in an unknown medium
Imaging an unknown object in an unknown medium
No more multiple removal
No more multiple removal: Construct Primaries then Migrate
Improved surface-wave response from ambient noise in Malargüe, Argentina, using seismic interferometry by multidimensional deconvolution
Improved surface-wave response from ambient noise in Malargüe, Argentina, using seismic interferometry by multidimensional deconvolution
Application of seismic interferometry by multidimensional deconvolution to ambient seismic noise recorded in Malargüe, Argentina
Application of seismic interferometry by multidimensional deconvolution to ambient seismic noise recorded in Malargüe, Argentina
Coda-wave interferometry and the Marchenko method
Coda-wave interferometry and the Marchenko method
Layer-specific imaging and monitoring in the Groningen subsurface using seismic interferometry
Layer-specific imaging and monitoring in the Groningen subsurface using seismic interferometry
Practical considerations for the creation of virtual sources and receivers in the 3D subsurface
Practical considerations for the creation of virtual sources and receivers in the 3D subsurface
Homogeneous Green’s function retrieval using the Marchenko method
Homogeneous Green’s function retrieval using the Marchenko method
Subsurface monitoring using virtual sources and receivers
Subsurface monitoring using virtual sources and receivers
Data-driven retrieval of primary plane-wave responses
Data-driven retrieval of primary plane-wave responses
Imaging the earth's interior with virtual sources and receivers
Imaging the earth's interior with virtual sources and receivers
Do we need up/down decomposition for Marchenko imaging?
Do we need up/down decomposition for Marchenko imaging?
Marchenko without up/down decomposition on the Marmousi model and retrieval of the refracted waves: Are they caused by the Marchenko algorithm?
Marchenko without up/down decomposition on the Marmousi model and retrieval of the refracted waves: Are they caused by the Marchenko algorithm?
Discerning small time-lapse traveltime changes by isolating the seismic response of a reservoir using the Marchenko method
Discerning small time-lapse traveltime changes by isolating the seismic response of a reservoir using the Marchenko method
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