Within ray theory, travel times are sensitive to the medium only along
the ray path. If the arrival time is defined to be the point where th
e observed seismogram crosses a nonzero threshold, time domain computa
tions using Born scattering in a homogeneous unbounded medium show tha
t the sensitivity is large within a considerable volume, and most inte
nse near the source and receiver. Details of this volume or ''tube'' d
epend on the threshold value, the source time function and the instrum
ent response. Generally, as the threshold value gets larger, the volum
e of sensitivity and magnitude of sensitivity get larger. If the sourc
e time function is oscillatory, the region of highest sensitivity can
be quite complex. Due to the high sensitivity near the endpoints, ray-
theoretical tomography is likely to alias near-source and near-receive
r structure to produce spurious structure along the ray path.