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Geoscience Interpretation Visualization Consortium (GIVC)
GIVC Consortium Brochure PDF, 1.4 MB
The Geoscience Interpretation Visualization Consortium is focused on
computer aided stratigraphic interpretation of seismic volumes. In its
first few years, the consortium is conducting research to develop
processes and techniques for semi-automatic and automatic interpretation
of depositional systems.
Computer-aided structural interpretation has been embodied in tools in interactive
interpretation systems for a number of years. Since the early 1980s, horizon
autotracking tools have been available to help increase the speed and consistency
of horizon interpretation in 3-D seismic surveys. More recently, techniques have
been developed to provide computer-aided interpretation of faults and automatic
fault interpretation.
Computer tools to aid in stratigraphic interpretation of seismic volumes have developed
much more slowly. Horizon slicing has provided better images of depositional systems
since the mid-to-late 1980s. Proportional slicing or stratal slicing (mid 1990s) provides
even better imaging of depositional systems, and better discrimination between stacked
channel systems in the seismic data because these surfaces typically are a better
approximation of paleo-depositional surfaces than horizon slices or time slices.
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The Geoscience Interpretation Visualization Consortium, which began in 2003, is
conducting R&D to develop a process for semi-automatic extraction of channels, reefs,
and other depositional features from seismic volumes. This process consists of:
- Filtering to remove random noise while preserving edges in the data.
- "Tunable" continuity calculations to selectively maximize imaging of faults,
channels, reefs, etc.

- Patented process using 2-D and 3-D algorithms to automatically extract
3-D fault surfaces from continuity volumes
- Creates two new attribute volumes:
- Lineament Enhanced Volume - probability estimate that voxel is part of a lineament
- Fault Enhanced Volume - probability estimate that voxel is part of a fault surface
- Extracts 3-D fault surfaces as named linked sets of polylines
- Perform a coordinate transformation from (x,y,t) to
(x,y, stratal slice) on the seismic volume
- Transformation honors interpreted horizons, faults, and a
variety of geological intervals (e.g., growth interval, carbonate platform, …)
Growth interval with dipping normal fault
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Stratal-sliced transformed data honoring vertical component of fault displacement
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- Calculate attributes designed to image stratigraphic features and depositional
systems using the stratal-sliced volume as input, including continuity "tuned" to
image stratigraphic features/depositional systems.
Continuity tuned for channels
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Continuity tuned for faults
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- Morphological Segmentation
- Use a modified form of AFE to extract depositional features
as linked sets of polylines
- Growing Neural Gas (GNG) for Seismic Facies Analysis and Segmentation
- Apply GNG to combinations of attribute volumes for seismic facies analysis in 3-D
- Segment 3-D geobodies by selecting clusters of nodes/data in state space with GNG
- Create the bounding surface for the extracted geobody
Interpreter defined starting surface around the geobody
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"Shrink-wrapped" geobody bounding surface
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- Apply the inverse of the stratal-slice transformation to
the extracted geobody bounding surfaces.
- Integrated these transformed bounding surfaces into the
display of the seismic volume in (x,y,t).
- Inverse transformation honors interpreted horizons, faults,
and a variety of geological intervals (e.g., growth interval, carbonate platform, …)
Consortium membership is $50,000 and provides the
following benefits:
- Input on research directions and focus of GIVC.
- GIVC research results (reports, algorithms, open source code).
- Evaluation copies of current software for fault extraction.
- Company affiliation with rights to participate in the Advisory Committee
meetings, transfer technology through the Visiting Scientist program, and
otherwise interact with the company's staff and facilities.
Consortium meetings are held twice a year. The first meeting is used to
review current consortium deliverables and discuss current industry needs.
In addition the year's research agenda is planned.
The second meeting is held mid-year to review projects' status and deliver
interim results.
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