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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: Case Studies Using Sequence Stratigraphy on an Interactive 3-D Seismic
Workstation
By
1The Energists
2Landmark Graphics Corporation
Interpretation of 2-D and 3-D seismic data using workstations has greatly enhanced our exploration and exploitation efforts. The ratios of successful/nonsuccessful wells have improved, and finding costs have been reduced. The primary emphasis of these efforts has been structural interpretations, however. This has been dictated largely by the available software. The stratigraphic component has been underutilized and not exploited. Review of many case histories that describe the traps as being structural shows stratigraphy to be a significant component of the traps.
Stratigraphic analysis of seismic data on
workstations is now possible; software is
available from several sources. We have
applied these tools to interpretation problems
in the Gulf of Mexico, North Sea,
North Africa, South America, and southeast
Asia. The methodology involves describing
and assigning values for seismic
attributes such as the external geometry,
internal reflection configuration, amplitude,
and continuity to areas bounded horizontally
by horizons and vertically by internal
partitions ("schzaa M" lines). These attributes
and well data are used to make
lithofacies,
systems
tracts
, and depositional
environment predictions for each interval
of interest. The predictions are then interactively
projected to map view. Their values
are electronically contoured to produce
maps of the seismic facies, external geometry,
continuity, amplitude,
systems
tracts
,
lithofacies, and depositional environments;
these can easily be plotted at various scales.
It is also possible to effect a
chronostratigraphic analysis and restore
missing intervals.
We will present case histories from the Gulf
of Mexico and North Sea that will show
the application of these
types
of analyses
to carbonate ramps, deltaic clastics, submarine
fans, and basin inversion and erosion.
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