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A notable exception to the repeatable nature of the overburden
is the thin anomaly in the migration difference section at the
center of the profile, labeled ``B'' at about 750 ms pseudodepth.
This anomaly may be the effect of a steam leak in the shallow portion
of the injection well. The subsequent heating and desaturation
around the borehole region would be likely to cause such a narrow vertical band
of time delay in the center of the profile. Later migration profiles
show this region to extend vertically with calendar time.
Next: Steam zone diffractions
Up: IMAGES OF FLUID FLOW
Previous: Repeatability
Stanford Exploration Project
11/12/1997