40 citations · 329 across the 47 of their papers we have counts for
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Representations for multidimensional down-down deconvolution of ocean-bottom seismic data: theory and practical implications
Kees Wapenaar, Matteo Ravasi, Claudio Bagaini
Multidimensional up-down deconvolution effectively eliminates surface-related multiples from ocean-bottom seismic data. Recently, several down-down deconvolution methods have been…
Reciprocity and representation theorems for rotational seismology
Kees Wapenaar
Recently, there has been an increasing interest in employing rotational motion measurements for seismic source inversion, structural imaging and ambient noise analysis. We derive r…
Multiple reflections on Huygens' principle
Kees Wapenaar
According to Huygens' principle, all points on a wave front act as secondary sources emitting spherical waves, and the envelope of these spherical waves forms a new wave front. In…
Recursive Interferometric Surface-wave Suppression For Improved Reflection Imaging
Faezeh Shirmohammadi, Deyan Draganov, Ranajit Ghose +3
High-resolution seismic reflections are essential for imaging and monitoring applications. In seismic land surveys using sources and receivers at the surface, surface waves often d…
On acoustic space-time media that compute their own inverse
Dirk-Jan van Manen, Johannes Aichele, Jonas Müller +2
We derive time reflection and transmission coefficients for 1D acoustic waves encountering a time boundary at which the properties of the medium change instantaneously. The time re…
Application of virtual seismology to DAS data in Groningen
Johno van IJsseldijk, Musab Al Hasani, Eric Verschuur +2
In this report we investigate whether and under what conditions virtual seismology via the acoustic Marchenko method can be applied to DAS data from a survey in the province of Gro…
Design, implementation and application of the Marchenko Plane-wave algorithm
Jan Thorbecke, Mohammed Almobarak, Johno van IJsseldijk +3
The Marchenko algorithm can suppress the disturbing effects of internal multiples that are present in seismic reflection data. To achieve this, a set of coupled equations with four…
Target-oriented least-squares reverse-time migration with Marchenko redatuming and double-focusing: Field data application
Aydin Shoja, Joost van der Neut, Kees Wapenaar
Recently, the focus of reflection seismologists has shifted to applications where a high-resolution image of the subsurface is required. Least-Squares Reverse-Time Migration (LSRTM…
The role of the background velocity model for the Marchenko focusing of reflected and refracted waves
Mert Sinan Recep Kiraz, Roel Snieder, Kees Wapenaar
Marchenko algorithms retrieve the wavefields excited by virtual sources in the subsurface, these are the Green's functions consisting of the primary and multiple reflected waves. T…
On evanescent wave field retrieval with the Marchenko method in 2D settings
Joeri Brackenhoff, Kees Wapenaar
We show the capability of the Marchenko method to retrieve not only propagating waves, but also evanescent waves, based on a recent derivation of the Marchenko method that does not…
Application of Marchenko-based isolation to a land S-wave seismic dataset
Faezeh Shirmohammadi, Deyan Draganov, Johno van IJsseldijk +4
The overburden structures often can distort the responses of the target region in seismic data, especially in land datasets. Ideally, all effects of the overburden and underburden…
A framework for subsurface monitoring by integrating reservoir simulation with time-lapse seismic surveys
Johno van IJsseldijk, Hadi Hajibeygi, Kees Wapenaar
Reservoir simulations for subsurface processes play an important role in successful deployment of geoscience applications such as geothermal energy extraction and geo-storage of fl…
Time-lapse applications of the Marchenko method on the Troll field
Johno van IJsseldijk, Joeri Brackenhoff, Jan Thorbecke +1
The data-driven Marchenko method is able to redatum wavefields to arbitrary locations in the subsurface, and can, therefore, be used to isolate zones of specific interest. This cre…
Target-Enclosed Least-Squares Seismic Imaging
Aydin Shoja, Joost van der Neut, Kees Wapenaar
Least-Squares Reverse-Time Migration (LSRTM) is a method that seismologists utilize to compute a high-resolution subsurface image. Nevertheless, LSRTM is a computationally demandin…
Propagator and transfer matrices, Marchenko focusing functions and their mutual relations
Kees Wapenaar, Marcin Dukalski, Christian Reinicke +1
Many seismic imaging methods use wave field extrapolation operators to redatum sources and receivers from the surface into the subsurface. We discuss wave field extrapolation opera…
Target-oriented least-squares reverse-time migration using Marchenko double-focusing: reducing the artifacts caused by overburden multiples
Aydin Shoja, Joost van der Neut, Kees Wapenaar
Geophysicists have widely used Least-squares reverse-time migration (LSRTM) to obtain high-resolution images of the subsurface. However, LSRTM needs an accurate velocity model simi…
Extracting small time-lapse traveltime changes in a reservoir using primaries and internal multiples after Marchenko-based target zone isolation
Johno van IJsseldijk, Joost van der Neut, Jan Thorbecke +1
Geophysical monitoring of subsurface reservoirs relies on detecting small changes in the seismic response between a baseline and monitor study. However, internal multiples, related…
On the relation between the propagator matrix and the Marchenko focusing function
Kees Wapenaar, Sjoerd de Ridder
The propagator matrix "propagates" a full wave field from one depth level to another, accounting for all propagation angles and evanescent waves. The Marchenko focusing function fo…
Green's function representations for Marchenko imaging without up/down decomposition
Kees Wapenaar, Roel Snieder, Sjoerd de Ridder +1
Marchenko methods are based on integral representations which express Green's functions for virtual sources and/or receivers in the subsurface in terms of the reflection response a…
3D virtual seismology
Joeri Brackenhoff, Jan Thorbecke, Kees Wapenaar
We create virtual sources and receivers in a 3D subsurface using the previously derived single-sided homogeneous Green's function representation. We employ Green's functions and fo…
Elastodynamic single-sided homogeneous Green's function representation: Theory and numerical examples
Christian Reinicke, Kees Wapenaar
The homogeneous Green's function is the difference between an impulse response and its time-reversal. According to existing representation theorems, the homogeneous Green's functio…
The Marchenko method for evanescent waves
Kees Wapenaar
With the Marchenko method, Green's functions in the subsurface can be retrieved from seismic reflection data at the surface. State-of-the-art Marchenko methods work well for propag…
Adaptation of the iterative Marchenko scheme for imperfectly sampled data
Johno van IJsseldijk, Kees Wapenaar
The Marchenko method retrieves the responses to virtual sources in the Earth's subsurface from reflection data at the surface, accounting for all orders of multiple reflections. Th…
3D Marchenko internal multiple attenuation on narrow azimuth streamer data of the Santos Basin, Brazil
Myrna Staring, Kees Wapenaar
In recent years, a variety of Marchenko methods for the attenuation of internal multiples has been developed. These methods have been extensively tested on 2D synthetic data and ap…