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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: Geochemical Logic and Techniques for
Unconventional
Gas
Exploration
Gas
ExplorationBy
Humble Geochemical Services
Source rocks have been oil productive for many years, typically
from highly fractured units or from adjacent porous intervals.
In addition source rocks may be good resources for
gas
if they
have the optimal organic richness and
thermal maturity necessary to have
converted both residual kerogen and any
retained oil to
gas
. Obviously, completion
engineering is a critical component of
extracting the
gas
from these systems, but
commercial rates will not be achieved if a
minimum level of conversion or thermal
maturity has not been reached.
While
gas
is generated in the oil window from all kerogen types
(whether oil or
gas
prone), the presence of black oil components
will occlude the limited permeability of a tight shale system,
resulting in low flow rates and precipitous decline rates. Thus,
even though
gas
shows are present in the oil window and measured
gas
contents can appear commercial, it does not necessarily
indicate the likelihood of commercial shale
gas
production.
Gas
window thermal maturity is a critical component of producibility
as the presence of higher molecular black oil components will
occlude the limited permeability of a tight source rock and result
in low
gas
flow rates.
Thermal maturity should be assessed by both visual and chemical
means. Visual methods such as vitrinite reflectance are the most
common means and are widely used. Oftentimes, however,
vitrinite reflectivity is not the best indication of the presence of
producible
gas
from tight rocks. These
data
should be complemented
by
data
obtained
through chemical techniques. These
techniques include Rock-Eval Tmax,
kerogen transformation ratio,
gas
composition,
carbon isotopes, and residual liquids
fingerprinting. Using these techniques, the
extent of organic matter conversion to
gas
can be accurately determined. The key point
is that indications of thermal maturity
may not necessarily agree with the extent
of kerogen conversion, nor provide a
good indication of the presence of
problematic compounds.
Gas
risking plots can then be
constructed to ascertain if all
data
provide a consistent
assessment of
gas
producibility.
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