| WHAT
IS WELL-LOG SEQUENCE STRATIGRAPHY? |
|
- Well-log
Sequence Stratigraphic analysis is a methodology that permits
a geologist and geophysicist to subdivide a stratigraphic section
into a series of time related 3rd Order Depositional Sequences
and Systems Tracts.
- This is
accomplished by the integration of High Resolution
Biostratigraphic analysis, marker species, abundance and diversity
histograms, paleobathymetry and paleoenvironment correlated with
well log signatures.
- Wells with
Well-Log Sequence Stratigraphic analysis can be
correlated by MICRO-STRAT INC. to 2-D and 3-D seismic.
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| APPLICATIONS
OF WELL-LOG SEQUENCE STRATIGRAPHY |
- Establish
reference wells with Sequence Boundaries, Maximum Flooding Surfaces
and Systems Tracts that can be age-dated (Ma) and correlated with
the Global Cycle Chart.
- Determine
timing of faults, unconformities, canyon development, salt intrusion,
reef development, migration, maturation and seals for hydrocarbons.
- Graphic
correlation plots; help recognize the sequence boundaries and
maximum flooding surfaces.
- Prediction
of ages and surfaces ahead of the drill bit.
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| WELL-LOG
SEQUENCE STRATIGRAPHY WILL HELP YOU TO: |
- Identify
the 3rd Order Depositional Sequences and Systems Tracts that are
associated with the potential hydrocarbon reservoirs, source rocks
and seals.
- Determine
the play concepts for the reservoir section, coastal belt sands,
shingled turbidites sands, sheet sands, and channel overbank sands
(parallel to strike): incised valley fill sands and slope fan
channel sands, (perpendicular to strike) and basin floor fan sands
that form pancake shaped reservoir.
- Predict
the geometry, continuity and distribution of the reservoir sands
both vertically and laterally.
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NOTE:Tops
only reports include Well-Log Sequence Stratigraphy with marker
species, numerical ages, paleowater depth, well-log, Sequence Boundaries,
Maximum Flooding Surfaces and Systems Tract boundaries.
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