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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: High-Resolution Sequence Stratigraphy
Using
Well
Logs and Cores
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Sequence stratigraphy is the study of sedimentary
rocks within a framework of genetically related facies
bounded by chronostratigraphicaly significant surfaces.
Using the concepts of sequence stratigraphy, it is possible
to construct a high-resolution chronostratigraphic framework
from well
logs, cores, and outcrops for the analysis of
reservoir, source, and sealing rocks at a reservoir to
regional scale.
The sequence is the fundamental stratal unit for a sequence stratigraphic analysis. Sequence boundaries are areally continuous surfaces within a basin, interpreted to form as a result of a eustatic fall (Vail et al, 1977). The sequence boundary is overlain and underlain by rocks of different ages; but all of the rocks above the boundary are younger than all the rocks below the boundary, so the boundary has time-stratigraphic significance.
There is a distinct break in deposition and a basinward
shift in facies across the unconformable portion of a type-1
sequence boundary, making it a natural surface for separating
facies above and below. Recognition of sequence
boundaries on well
-log cross sections is essential for accurate
lateral and vertical facies analysis leading to reservoir
mapping and distribution prediction.
Parasequences are the building blocks of the sequence.
Aggradational, progradational, and retrogradational
stacking patterns of parasequences are used to subdivide
the sequence into systems tracts. Parasequence boundaries
are locally continuous surfaces interpreted to form as a
result of a relative rise in sea-level, and are ultra high-resolution
chronostratigraphic surfaces used to correlate
time and facies from well
logs within a sequence framework.
Integration of sequence and parasequence correlation
concepts provides techniques to look at basins in fresh ways
resulting in: 1) definition of new play types
, opening up
heavily drilled basins for new exploration, 2) improved
ability to define and locate subtle, but potentially profitable
stratigraphic traps, and 3) a more integrated stratigraphic
framework for risking new plays.
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