TY - GEN
T1 - Discriminating physical and non-physical energy in wavefield interferometry
AU - Meles, G. A.
AU - Curtis, A.
N1 - Publisher Copyright:
Copyright © (2012) by the European Association of Geoscientists & Engineers All rights reserved.
PY - 2013
Y1 - 2013
N2 - Source-receiver interferometry is a technique that allows the Green's functions between sources and receivers to be estimated by means of convolution and cross-correlation of other recorded wavefields. Source-receiver interferometry has been observed to work surprisingly well in practical applications when theoretical requirements (e.g. closed surrounding boundaries of other sources and receivers) are contravened: this paper contributes to explain why this may be true. Commonly-used inter-receiver interferometry requires wavefields to be generated around specific stationary points on the boundaries which are controlled purely by medium heterogeneity and receiver locations. By contrast, we show that source-receiver interferometry constructs at least kinematically correct physically scattered waves between a source and receiver by convolution of scattered data from and to any and all points on the boundary. This reduces the ambiguity in interpreting wavefields generated using source-receiver interferometry with only partial boundaries (as is standard in practical applications), as it allows spurious or non-physical events in the constructed Green's function to be identified and either interpreted or ignored.
AB - Source-receiver interferometry is a technique that allows the Green's functions between sources and receivers to be estimated by means of convolution and cross-correlation of other recorded wavefields. Source-receiver interferometry has been observed to work surprisingly well in practical applications when theoretical requirements (e.g. closed surrounding boundaries of other sources and receivers) are contravened: this paper contributes to explain why this may be true. Commonly-used inter-receiver interferometry requires wavefields to be generated around specific stationary points on the boundaries which are controlled purely by medium heterogeneity and receiver locations. By contrast, we show that source-receiver interferometry constructs at least kinematically correct physically scattered waves between a source and receiver by convolution of scattered data from and to any and all points on the boundary. This reduces the ambiguity in interpreting wavefields generated using source-receiver interferometry with only partial boundaries (as is standard in practical applications), as it allows spurious or non-physical events in the constructed Green's function to be identified and either interpreted or ignored.
UR - https://www.scopus.com/pages/publications/84930427297
U2 - 10.3997/2214-4609.20130954
DO - 10.3997/2214-4609.20130954
M3 - Conference contribution
AN - SCOPUS:84930427297
T3 - 75th European Association of Geoscientists and Engineers Conference and Exhibition 2013 Incorporating SPE EUROPEC 2013: Changing Frontiers
SP - 2701
EP - 2705
BT - 75th European Association of Geoscientists and Engineers Conference and Exhibition 2013 Incorporating SPE EUROPEC 2013
PB - European Association of Geoscientists and Engineers, EAGE
T2 - 75th European Association of Geoscientists and Engineers Conference and Exhibition 2013 Incorporating SPE EUROPEC 2013: Changing Frontiers
Y2 - 10 June 2013 through 13 June 2013
ER -