S(t,x)=S*(t,x)+E(t,x)
where ``model-consistent'' means as beforeSince there are several data running around in this part of the discussion, include the name of the data in the notation for the differential semblance objective:
J0[v,S]=J0[v.S*]+J0[v,E]+K[v,S*,E]
whereLikewise,
Suppose that u (or its corresponding v) is a stationary point of
J0[v,S], i.e. . Then
Theorem: At a stationary point of the differential semblance
objective, its value is bounded by a -uniform multiple of the
distance of the data to the set of model-consistent data.
Thus for a family of data converging to model-consistent data, any set of corresponding stationary points of J0 must have J0 values which converge to zero, modulo asymptotic errors.
This result may well not imply that stationary points for noisy data are global minima. Indeed, substitute the ``target'' velocity v* in the expression for J0[v,S]: from the expansion and estimates above you easily see that
In the next section I will show that when the differential semblance minimization is supplemented with proper constraints on the velocity model, in addition to those already imposed, the error in the RMS square slowness is proportional to the error in the data. It then follows from the estimates above that stationary values conforming to these constraints are indeed proportional to the square of the error level, hence essentially global minima. It would be interesting to know whether relaxing these constraints actually permits anomalously large stationary values.