Rj. Michelena et al., CROSSWELL TOMOGRAPHIC ESTIMATION OF ELASTIC-CONSTANTS IN HETEROGENEOUS TRANSVERSELY ISOTROPIC MEDIA, Geophysics, 60(3), 1995, pp. 774-783
The procedure to estimate elastic constants of a transversely isotropi
c medium from limited-aperture traveltimes has two steps. First, P- an
d SV-wave traveltimes are fitted with elliptical velocity functions ar
ound one of the axes of symmetry. Second, the parameters that describe
the elliptical velocity functions are transformed analytically into e
lastic constants. When the medium is heterogeneous, the process of fit
ting the traveltimes with elliptical velocity functions is performed t
omographically, and the trans-formation to elastic constants is perfor
med locally at each position in space. Crosswell synthetic and field d
ata examples show that the procedure is accurate as long as the data a
perture is constrained as follows: it should not be too large otherwis
e the elliptical approximation may not be adequate, and it should not
be too small because the tomographic estimation of elliptical velociti
es fails, even if the medium is actually isotropic.