TY - GEN
T1 - Point and edge diffractions in three dimensions
AU - Klokov, A.
AU - Baina, R.
AU - Landa, E.
PY - 2011
Y1 - 2011
N2 - Small geological objects - faults, fractures, karst, etc. - are presented by the diffracted component in the wavefield registered by seismic survey. Diffraction events analysis allows getting information about these objects. It this study we demonstrate how diffraction events behave in the migrated dip-angle domain. Using synthetic and real data we show that the event shape analysis makes it possible to detect a single diffraction point position, fractures direction and fault orientation.
AB - Small geological objects - faults, fractures, karst, etc. - are presented by the diffracted component in the wavefield registered by seismic survey. Diffraction events analysis allows getting information about these objects. It this study we demonstrate how diffraction events behave in the migrated dip-angle domain. Using synthetic and real data we show that the event shape analysis makes it possible to detect a single diffraction point position, fractures direction and fault orientation.
UR - http://www.scopus.com/inward/record.url?scp=80052460791&partnerID=8YFLogxK
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AN - SCOPUS:80052460791
SN - 9781617829666
T3 - 73rd European Association of Geoscientists and Engineers Conference and Exhibition 2011: Unconventional Resources and the Role of Technology. Incorporating SPE EUROPEC 2011
SP - 429
EP - 433
BT - Society of Petroleum Engineers - 73rd European Association of Geoscientists and Engineers Conference and Exhibition 2011 - Incorporating SPE EUROPEC 2011
PB - Society of Petroleum Engineers
ER -