About SCA
and geoLOGIC
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Subsurfave Consultants & Associates, LLC
10255 Richmond Ave., Suite 300W
Houston, Texas 77042
Phone: +1.713.789.2444
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VELOCITY
The Missing Link
What
is the most important connection between geology and geophysics
What is the
most important connection between geology and geophysics? How
is real world depth related to seismic time measurement? The
link is that long ignored, much misunderstood, and often miscalculated
entity called VELOCITY. It is the most fundamental, and
also the most elusive, of all earth science parameters. Unfortunately,
the subject of velocity, and its attendant role in depth conversion,
has been a pariah for as long as any of us can remember. What
we heard for depth conversion was -"Use the nearest checkshot
survey". We knew it wasn't that simple, and inevitably mistakes
were made.
The three dimensional
interpretation of velocity is every bit as important as the interpretation
of seismic times. These two interpretations meld to give the
final I structural depth picture. And as a bonus, the interpretation
of velocity can give usi much more. The top and bottom of abnormal
subsurface pressure can be mapped. Coefficients derived from
the detailed analysis of interval velocities, and related to
sand/shale ratios, can be displayed in an aerial sense. The integrated
study of-seismic sonic and checkshot velocities, together with
correctly processed and interpreted time horizons and faults,
is the key to deriving accurate depth models, as shown in Figure
1

Fig. 1
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As an example, consider
the problem of converting three dimensional time surfaces and fault
planes to depth. The success of this operation depends on:
- The correctness
of the time interpretation and the accuracy with which the seismic
data were processed.
- The intelligence
which went into the building of an accurate earth velocity model.
It is this second
aspect which has been neglected for so many years. However, we now
possess, courtesy of recently developed software packages, computer
tools specifically designed to perform the manipulations that we should
have been doing all along. We are able, for instance, to 'insert' a
time horizon or fault surface from an interpretation -workstation into
a three dimensional cube of velocity, and then directly make the depth
conversion (See Figure 2). However, what is needed before this can
be done, is the velocity model itself.

Fig. 2
In order to transform
a time horizon to depth, we need to use a field comprised of accurate
vertical propagation velocities. It is incorrect to use raw processing
derived velocities, even if they happen to come from the processing
of a pre-stack depth migration. Appropriate velocity fields are formed
in the computer from carefully scrutinized and edited vertical checkshots.
Any horizontal component in the checkshot will compromise the result.
The problem, even with vertical checkshot derived velocities, is that
wells are often drilled in non-ideallocations for the purposes of good
velocity work. Structural highs and fault zones, which involve localized
anomalies in interval velocity, do not provide perfect velocity measurement
conditions. However, the checkshots are still the best data we have
for depth conversion purposes.
The construction
of an accurate velocity model requires that the time interpretation
be i an integral part of its formation. Whether the derived velocity
field is a simple cube or a more complex layered model, the success
of depth work still relies on the interpretation of the geologically
well informed geoscientist. In the end, exploration success depends
more than anything else on the accuracy of the depth model, and that
model is derived from interpretations of both time AND velocity.
Paul Kennedy |
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