TY - JOUR
T1 - Time preserving tomography
AU - Liram, Lior
AU - Naveh, Yoav
AU - Dekel, Gali
AU - Koren, Zvi
N1 - Publisher Copyright:
© 2014 SEG.
PY - 2014
Y1 - 2014
N2 - Time Preserving Tomography is an accurate, efficient and flexible tool for constructing kinematically equivalent subsurface models given a background model and a set of model parameter perturbations. In this method, parameters of the background model are allowed to change while preserving traveltimes of all ray pairs. Perturbations can be applied for all types of model parameters. In the case of tilted transverse isotropy (TTI) the model parameters are the axial compressional velocity, Thomsen anisotropic interval parameters epsilon and delta, and the depth values of the model horizons. The traveltimes of all ray pairs traced during the tomographic inversion are kinematic invariants. In the migrated domain, all the kinematically equivalent models should provide more or less flat reflection events along common image gathers (CIG). In fact, time-preserving tomography does not require CIG at all. An example of the application of this type of method is the use of misties between well markers and seismic depth horizons to obtain Thomsen delta parameters (Mancini, 2013). Timepreserving tomography is a very useful tool for depth interpretation, uncertainty analysis and risk management.
AB - Time Preserving Tomography is an accurate, efficient and flexible tool for constructing kinematically equivalent subsurface models given a background model and a set of model parameter perturbations. In this method, parameters of the background model are allowed to change while preserving traveltimes of all ray pairs. Perturbations can be applied for all types of model parameters. In the case of tilted transverse isotropy (TTI) the model parameters are the axial compressional velocity, Thomsen anisotropic interval parameters epsilon and delta, and the depth values of the model horizons. The traveltimes of all ray pairs traced during the tomographic inversion are kinematic invariants. In the migrated domain, all the kinematically equivalent models should provide more or less flat reflection events along common image gathers (CIG). In fact, time-preserving tomography does not require CIG at all. An example of the application of this type of method is the use of misties between well markers and seismic depth horizons to obtain Thomsen delta parameters (Mancini, 2013). Timepreserving tomography is a very useful tool for depth interpretation, uncertainty analysis and risk management.
UR - http://www.scopus.com/inward/record.url?scp=85018393580&partnerID=8YFLogxK
U2 - 10.1190/segam2014-0116.1
DO - 10.1190/segam2014-0116.1
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AN - SCOPUS:85018393580
SN - 1052-3812
VL - 33
SP - 4793
EP - 4797
JO - SEG Technical Program Expanded Abstracts
JF - SEG Technical Program Expanded Abstracts
T2 - SEG Denver 2014 Annual Meeting, SEG 2014
Y2 - 26 October 2011 through 31 October 2011
ER -