Výsledky vyhledávání - "Brackenhoff, J.A."

Subsurface monitoring using virtual sources and receivers

Autor: Brackenhoff, J.A., Thorbecke, J.W., Wapenaar, C.P.A.

Publikováno v: AGU Fall Meeting. Online due to COVID-19
AGU Fall Meeting

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Practical considerations for the creation of virtual sources and receivers in the 3D subsurface

Autor: Brackenhoff, J.A., Thorbecke, J.W., Wapenaar, C.P.A.

Publikováno v: AGU Fall Meeting 2019. San Francisco, United States
AGU Fall Meeting 2019

In recent years, progress has been made in the field of virtual seismology. Using the novel data-driven Marchenko method, virtual sources and receivers can be created in the subsurface using only reflection data at the surface of the Earth and a back

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Virtual seismology: from hydrocarbon reservoir imaging to induced earthquake monitoring

Autor: Wapenaar, C.P.A., Brackenhoff, J.A., Staring, M., Thorbecke, J.W., Slob, E.C.

Publikováno v: Proceedings of the American Geophysical Union (AGU) Fall Meeting 2018

Recent developments in exploration seismology have enabled the creation of virtual sources and/or virtual receivers in the subsurface from reflection measurements at the earth's surface. Unlike in seismic interferometry, no physical instrument (recei

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Homogeneous Green’s function retrieval using the Marchenko method

Autor: Brackenhoff, J.A., Thorbecke, J.W., Wapenaar, C.P.A.

Publikováno v: SIAM Houston Imaging Sciences Symposium. Houston, United States
SIAM Houston Imaging Sciences Symposium

In wave theory, a Green’s function is defined as the response of a medium to an impulsive point source. The homogeneous Green’s function is the combination of the Green’s function and its time-reversal. Homogeneous Green’s functions can be re

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Decomposition of the Green's function using the Marchenko equation

Autor: Brackenhoff, J.A., van der Neut, J.R., Wapenaar, C.P.A., Mihai Popovici, A., Fomel, S.

Publikováno v: Proceedings of the 87th SEG annual meeting, expanded abstracts

The Marchenko equation can be used to retrieve the Green’s function at depth as a full function or decomposed into its upand downgoing parts. We show that the equation can be rewritten to create a decomposition scheme that can decompose a full wave

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