Big ray-tracing and eikonal solver on unstructured grids: Application to the computation of a multivalued traveltime field in the Marmousi model

Citation
R. Abgrall et Jd. Benamou, Big ray-tracing and eikonal solver on unstructured grids: Application to the computation of a multivalued traveltime field in the Marmousi model, GEOPHYSICS, 64(1), 1999, pp. 230-239
Citations number
26
Categorie Soggetti
Earth Sciences
Journal title
GEOPHYSICS
ISSN journal
00168033 → ACNP
Volume
64
Issue
1
Year of publication
1999
Pages
230 - 239
Database
ISI
SICI code
0016-8033(199901/02)64:1<230:BRAESO>2.0.ZU;2-2
Abstract
This paper presents a numerical computation of the multivalued traveltime f ield generated by a point-source experiment in the Marmousi model. Two meth ods are combined to achieve this goal: a method called big ray tracing, use d to compute multivalued traveltime fields, and an eikonal solver, designed to work on unstructured meshes. Big ray tracing is based on a combination of ray tracing and local solution s of the eikonal equation. Classical ray tracing first discretizes the phas e space and defines local zones that possibly overlap where the traveltime field is multivalued. Then an eikonal solver computes traveltimes in these zones called big rays. It acts as an exact interpolation process between ra ys associated with different branches of the traveltime field. The geometry of big rays may be complicated and is better discretized using unstructure d meshes. An eikonal solver designed to work on unstructured meshes is used .