TY - GEN
T1 - Local angle domain in seismic imaging
AU - Koren, Z.
AU - Ravve, I.
AU - Bartana, A.
AU - Kosloff, D.
PY - 2007
Y1 - 2007
N2 - The Local Angle Domain (LAD) is a system of four angles defining the interaction between incident and reflected waves at a specifie image point (element). Two angles represent the spatial direction of the ray-pair normal: its dip (zenith) and azimuth. The two other angles define the reflection angle system. The third angle is the half-opening angle between the incident and the reflected rays. The definition of these three angles is conventional. We define the fourth LAD angle as the azimuth of the ray-pair plane measured in the ray-pair reflection surface. The LAD angles are defined in a rotated local frame, whose "vertical" axis coincides with the background (reference) normal of the reflection surface element. The forward and the inverse transforms between the directions of the incident and the reflected rays and the LAD angles are presented. We consider Isotropie and TTI anisotropic media, pressure waves and converted waves. The presented notation is used within ray-based and wave-equation angle domain migrations.
AB - The Local Angle Domain (LAD) is a system of four angles defining the interaction between incident and reflected waves at a specifie image point (element). Two angles represent the spatial direction of the ray-pair normal: its dip (zenith) and azimuth. The two other angles define the reflection angle system. The third angle is the half-opening angle between the incident and the reflected rays. The definition of these three angles is conventional. We define the fourth LAD angle as the azimuth of the ray-pair plane measured in the ray-pair reflection surface. The LAD angles are defined in a rotated local frame, whose "vertical" axis coincides with the background (reference) normal of the reflection surface element. The forward and the inverse transforms between the directions of the incident and the reflected rays and the LAD angles are presented. We consider Isotropie and TTI anisotropic media, pressure waves and converted waves. The presented notation is used within ray-based and wave-equation angle domain migrations.
UR - http://www.scopus.com/inward/record.url?scp=55549109454&partnerID=8YFLogxK
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AN - SCOPUS:55549109454
SN - 9781605601557
T3 - 69th European Association of Geoscientists and Engineers Conference and Exhibition 2007: Securing The Future. Incorporating SPE EUROPEC 2007
SP - 3031
EP - 3035
BT - 69th European Association of Geoscientists and Engineers Conference and Exhibition 2007
PB - Society of Petroleum Engineers
T2 - 69th European Association of Geoscientists and Engineers Conference and Exhibition 2007 - "Securing The Future"
Y2 - 11 June 2007 through 14 June 2007
ER -