Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
Source location by diffraction stacking. / Gajewski, D. J.; Anikiev, D.; Kashtan, B.; Tessmer, E.; Vanelle, C.
69th EAGE Conference & Exhibition incorporating SPE EUROPEC 2007: Abstracts . European Association of Geoscientists and Engineers, 2007. p. P215 cp-27-00461.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Source location by diffraction stacking
AU - Gajewski, D. J.
AU - Anikiev, D.
AU - Kashtan, B.
AU - Tessmer, E.
AU - Vanelle, C.
PY - 2007
Y1 - 2007
N2 - For deposits with weak 4-D signatures the passive seismic method may provide an alternative option for reservoir characterization. We introduce a new localization technique which does not require any picking of events in the individual seismograms of the recording network. The localization is performed by a modified diffraction stack of the squared amplitudes of the input seismograms resulting in the image section. The method is target oriented and is best suited for large networks of surface and/or downhole receivers. The source location is obtained from the maximum of the image section for the time window under consideration. Since the focusing analysis is performed only in this section, no optimized search procedures are required. The source time is determined in a second processing step after the source location. Initial tests with 2-D homogeneous media indicate the high potential of the method. Since the maximum of the image section is distinct even very weak events can be detected.
AB - For deposits with weak 4-D signatures the passive seismic method may provide an alternative option for reservoir characterization. We introduce a new localization technique which does not require any picking of events in the individual seismograms of the recording network. The localization is performed by a modified diffraction stack of the squared amplitudes of the input seismograms resulting in the image section. The method is target oriented and is best suited for large networks of surface and/or downhole receivers. The source location is obtained from the maximum of the image section for the time window under consideration. Since the focusing analysis is performed only in this section, no optimized search procedures are required. The source time is determined in a second processing step after the source location. Initial tests with 2-D homogeneous media indicate the high potential of the method. Since the maximum of the image section is distinct even very weak events can be detected.
U2 - 10.3997/2214-4609.201401879
DO - 10.3997/2214-4609.201401879
M3 - Conference contribution
SN - 9789073781542
SP - P215
BT - 69th EAGE Conference & Exhibition incorporating SPE EUROPEC 2007
PB - European Association of Geoscientists and Engineers
T2 - 69th EAGE Conference and Exhibition incorporating SPE EUROPEC 2007
Y2 - 11 June 2007 through 14 June 2007
ER -
ID: 4736411