Impact of Realistic Shale Properties on Exploration-Scale Vertical Migration Modeling
Dempster, Kelly, William Almon,
William Dawson, Michael Hertle, ChevronTexaco,
Basin modelers routinely incorporate data and interpretations
from other disciplines into their models: structural and seismic interpretation
for past and present geometry, log analysis for lithologic
content, sequence stratigraphy for depositional
framework and lithologic continuity, biostratigraphy for ages, and geochemistry for source rock
properties, thermal calibration, and migration indicators.
Seal behavior has historically been treated differently: instead
of adjusting the model inputs to reflect measured values, model results have
usually been compared after the fact to observed seal properties. Default shales in basin modeling programs have been designed to be
excellent top seals and to hold large hydrocarbon columns. In the early basin
models for the deep-water prospects in
The lack of fit
to observed occurrences of hydrocarbon required ChevronTexaco
to develop a methodology that incorporates measured shale/seal properties into
existing models. Analyses of marine shales reveal
six distinct groups, based on fabric and textural variations. Each type has a
different compaction rate, which influences seal character. This variation is
described in terms of porosity-depth and porosity-effective stress
relationships, porosity versus permeability, and capillary entry pressure
distributions. A regional database relates mudstone properties to sequence stratigraphic position and depositional setting. Data
relating interfacial tension to composition, as well as temperature and
pressure, are also captured.