NEW PLAY CONCEPTS IN STRUCTURAL
GEOLOGY
By:
Daniel J. Tearpock, Richard Bischke and Hines Austin
Quickly dismissing new ideas that
seem to depart from "established" procedures is not a good
idea. An established exploration concept is a good idea only
if it produces results. To paraphrase Parke A. Dickey's 1958
observation, "Several times in the past we thought we were running
out of oil: Actually, we were only running out of ideas".
One established method for finding
oil in extensional tectonic areas, like the United States Gulf
Coast, has been to drill hanging wall rollovers. This approach
has been so successful and common, that many companies believe
that all of the major rollovers have been drilled.
If drilling hanging wall rollovers
has been so successful, then why not try drilling sub-fault or
duplex rollovers?. These deeper extensional sub-fault plays may
have oil and gas potentials similar to currently producing rollovers.
A well-imaged example of a subfault rollover is shown in Figure
1. There is no lack of structures, but only a lack of new exploration
ideas.

Many reasons will be given for not
drilling these deeper plays, including: higher costs, lower porosity,
greater risk, poorer data, "We can't do thatl", "it has not been
done before", etc. However, if large amounts of hydrocarbons
exist at deeper levels, and we believe they do, then someone
will drill for and exploit these hydrocarbons.
One objection to drilling deeper is
poor data. New methods in structural geology have ho vsrever,expanded
our ability to predict structure even in poor data areas. For
example, did you ever see a large listric growth fault that did
not contain a large hanging wall rollover? |
There are predictable relationships between
the shape of a growth normal fault and the shape of thwe associated
rollover. In other words, if you know fault shape, then you can successfully
predict fold shape. How these processes work are described in several
of our past and pending publications, although some of our meiihods
are proprietary.
One observation we wish to point out is
that duplex faults commonly have low dips and therefore may image on
record sections (see Figures 9-60 and 9-62, in Applied Subsurface Geological
Mapping). These deeper rollovers have steeply dipping beds which do
not image on record sections.
We have the "breakthrough technology" to
employ the above and other new and tested methods of structural analysis,
to locate new structural plays. To explore for new types of plays a
company must innovate. A structural expert must be on staff, or available
as a consultant, who understands complex structural analysis.
Ongoing economic success often depends on
a company's ability to learn, understand, and apply new, productive,
and exciting play concepts.
CONTOUR
COMPATIBILITY
Structure maps on multiple horizons are
often created without regard to the three dimensional validity of the
interpretation as a whole. This can result in closely spaced structure
maps that imply radical changes in strike, dip or thickness in very
short intervals (Figure 2). The mapped horizons are only 90-95 feet
apart, but the 7100 foot contours on the two maps look like they may
cross just south of the map. This would make the deeper horizon shallower
than the shallow horizon. In areas of steep dip, structure maps that
are hundreds of feet apart can be miscontoured so that separate horizons
cross each other.

When reviewing maps, one excellent QLT is
to overlay the maps and verify that any changes in structure are reasonable
and compatible in three dimensions. In Figure 3, the closely spaced
horizons have similar strikes and dips. In steeply dipping areas, a
hand sketched cross section on the mapped horizons can quickly show
contouring problems. (Figure 4)


INCREASED WORKSTATION PRODUCTIVITY
Subsurface Consultants & Associates,
Inc. would like to introduce our newest associate "Computer Aided Technological
Services", specialists in workstation technology. C.A.T.S. has a different
approach to 3-D workstation interpretation, managing a project from
start to finish wholly within the seismic interpretation environment.
Whereas others require two or three different software packages, typically,
to interpret seismic data, integrate subsurface information, and construct
a depth controlled structure map.
C.A.T.S. uses a proprietary database interface
to add subsurface integration capabilities to the standard Landmark
seismic interpretation software. In addition, advanced interpretation
techniques, and innovative mapping techniques, as presented in the
textbook "Applied Subsurface Geological Mapping", increase productivity
and allow the production of show quality maps in the seismic environment.
This approach allows us to perform the geologic and geophysical tasks
in a common software environment. The result is unprecedented integration
of geologic and geophysical data, increased accuracy, and lower overall
costs. The accompanying display (Figure 5) is a portion of a map produced
totally within the Landmark seismic interpretation environment. 'Through
our new associate, we can now provide expanded seismic workstation
services. The combination of advanced structural methods and innovative
3-D workstation techniques is a hard combination to beat.

ENGINEERING
ROLE IN A FIELD STUDY
A field study is a synergistic effort involving
engineering, geologic and geophysical personnel in an interactive and
joint effort to locate, quantify and develop a plan to deplete the
remaining oil and gas reserves on a property. The engineer incorporates
production performance into the evaluation of the field. In the process
the engineer verifies and modifies the geologic interpretation of the
field, the rock and fluid properties, and recovery factors used to
determine the reserves in the field.
Finally, the engineer develops a performance
oriented plan to produce, workover, re-complete, test and develop all
the remaining proved and probable reserves. The optimum plan focuses
on maximizing profit and not just recovering reserves.
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