TY - JOUR
T1 - Marchenko-Based Target Replacement, Accounting for All Orders of Multiple Reflections
AU - Wapenaar, Kees
AU - Staring, Myrna
PY - 2018/6/1
Y1 - 2018/6/1
N2 - In seismic monitoring, one is usually interested in the response of a changing target zone, embedded in a static inhomogeneous medium. We introduce an efficient method that predicts reflection responses at the Earth's surface for different target-zone scenarios, from a single reflection response at the surface and a model of the changing target zone. The proposed process consists of two main steps. In the first step, the response of the original target zone is removed from the reflection response, using the Marchenko method. In the second step, the modelled response of a new target zone is inserted between the overburden and underburden responses. The method fully accounts for all orders of multiple scattering and, in the elastodynamic case, for wave conversion. For monitoring purposes, only the second step needs to be repeated for each target-zone model. Since the target zone covers only a small part of the entire medium, the proposed method is much more efficient than repeated modelling of the entire reflection response.
AB - In seismic monitoring, one is usually interested in the response of a changing target zone, embedded in a static inhomogeneous medium. We introduce an efficient method that predicts reflection responses at the Earth's surface for different target-zone scenarios, from a single reflection response at the surface and a model of the changing target zone. The proposed process consists of two main steps. In the first step, the response of the original target zone is removed from the reflection response, using the Marchenko method. In the second step, the modelled response of a new target zone is inserted between the overburden and underburden responses. The method fully accounts for all orders of multiple scattering and, in the elastodynamic case, for wave conversion. For monitoring purposes, only the second step needs to be repeated for each target-zone model. Since the target zone covers only a small part of the entire medium, the proposed method is much more efficient than repeated modelling of the entire reflection response.
KW - multiples
KW - representations
KW - seismic
KW - time-lapse
UR - http://resolver.tudelft.nl/uuid:13bf575c-66d4-4321-9329-29e99403660e
UR - http://www.scopus.com/inward/record.url?scp=85050190676&partnerID=8YFLogxK
U2 - 10.1029/2017JB015208
DO - 10.1029/2017JB015208
M3 - Article
AN - SCOPUS:85050190676
VL - 123
SP - 4942
EP - 4964
JO - JGR Solid Earth
JF - JGR Solid Earth
SN - 2169-9356
IS - 6
ER -