TY - GEN
T1 - Incomplete boundaries and partial equations in source-receiver interferometry (SRI)
AU - Löer, Katrin
AU - Meles, Giovanni A.
AU - Curtis, Andrew
PY - 2013/8/19
Y1 - 2013/8/19
N2 - Source-receiver interferometry (SRI) refers to a technique to construct the Green's function between a source and a receiver using only energy that has travelled from and to surrounding boundaries of sources and receivers. When the full boundary requirements for seismic interferometry are violated, spurious or non-physical energy is introduced into Green's function estimates. Using an acoustic model of a homogeneous medium embedding a single scatterer, we analyse the properties of the interferometric estimate for the case of a partial boundary located on one side of our model, as is commonly the case in practical experiments. We find, that it can be favourable, rather than a shortcoming, to use incomplete boundaries in order to preserve the information from non-physical arrivals that help to constrain the location of a scattering perturbation. Moreover, we show that one term of the SRI equation for scattering media is associated with standard imaging (migration) methods, and that for this term using a partial boundary is an advantage since this suppresses non-physical energy that might otherwise distort the image.
AB - Source-receiver interferometry (SRI) refers to a technique to construct the Green's function between a source and a receiver using only energy that has travelled from and to surrounding boundaries of sources and receivers. When the full boundary requirements for seismic interferometry are violated, spurious or non-physical energy is introduced into Green's function estimates. Using an acoustic model of a homogeneous medium embedding a single scatterer, we analyse the properties of the interferometric estimate for the case of a partial boundary located on one side of our model, as is commonly the case in practical experiments. We find, that it can be favourable, rather than a shortcoming, to use incomplete boundaries in order to preserve the information from non-physical arrivals that help to constrain the location of a scattering perturbation. Moreover, we show that one term of the SRI equation for scattering media is associated with standard imaging (migration) methods, and that for this term using a partial boundary is an advantage since this suppresses non-physical energy that might otherwise distort the image.
KW - acoustic
KW - scattering
KW - seismic
KW - numerical
UR - http://www.scopus.com/inward/record.url?scp=85058128352&partnerID=8YFLogxK
U2 - 10.1190/segam2013-1054.1
DO - 10.1190/segam2013-1054.1
M3 - Published conference contribution
AN - SCOPUS:85058128352
SN - 9781629931883
T3 - Society of Exploration Geophysicists
SP - 4579
EP - 4583
BT - SEG Technical Program Expanded Abstracts 2013
PB - Society of Exploration Geophysicists
T2 - Society of Exploration Geophysicists International Exposition and 83rd Annual Meeting: Expanding Geophysical Frontiers, SEG 2013
Y2 - 22 September 2013 through 27 September 2013
ER -