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Amoco TTI

Joe Dellinger

joe@sep.stanford.edu

ABSTRACT

Three versions of the University of Calgary's (FRP and CREWES jointly) overthrust physical model.

physical_model
the physical-model data This is the data we got from (University of Calgary - FRP and CREWES jointly) We got permission from them to include it in this distribution. If you use this data in a publication you should let them know about it beforehand and properly acknowledge them. This is the data used in the abstract: Prestack depth migration in TI media: examples with numerical and physical modeling data, Dai, Cheadle, and Isaac, GeoTriad convention 1998 abstracts, pages 83-84.
elastic
Amoco's synthetic elastic finite-difference version of their model. Mike O'brien calculated this model using a fully elastic 2D finite-difference modeling program of John Etgen's. Sam Gray and Bertrand Duquet provided the model dimensions and parameters. This data was used in the abstracts: Anisotropic true-amplitude migration, by Fei, Dellinger, Murphy, Hensley, and Gray. GeoTriad convention 1998 abstracts, pages 85-86, and SEG abstracts 1998 pages 1677-1679.
acoustic
Amoco's synthetic ISOTROPIC acoustic finite-difference version of their model. Mike O'brien calculated this model using an acoustic finite-difference modeling code of John Etgen's, using the P-wave velocities of the corresponding elastic model. (It uses the velocity normal to the layering in the anisotropic parts.) This version of the model, calculated using a single velocity and an acoustic code, is of course isotropic. For some unknown reason in this version of the model the reflector at the base was left out.

next up previous print clean
Next: Geometry of data Up: Vaillant: STANFORD EXPLORATION PROJECTElf Previous: Geometry of data
Stanford Exploration Project
1/15/2002