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
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
.