The elements of Bakken
Petroleum System consist of two source rocks
with high underlying burial depths for significant hydrocarbon generation.
However, this deep hydrocarbon generation process is dependent on
its kinetic properties, thermal maturity, and geochemical properties.
The statistical compensation effect is a complicating factor in the
kinetic analyses of the Bakken Formation. In this study, we experimentally
determined the kinetics of the Bakken formation source beds, observed
the presence of the residual compensation effect, and numerically
established a correlation between the kinetic parameters, thermal
maturity indices (
T
max
), and the vitrinite
reflectance (VR
o
) and bitumen reflectance (BR
o
). First, we conducted source rock analysis to determine kinetic
properties and the organic geochemical assays of reactive kerogen
in the Bakken source beds. Finally, we incorporated previous established
studies to generate numerical correlation for
T
max
in terms of VR
o
and BR
o
reflectance.
Our kinetic results show evidence of the residual compensation effect
in the Bakken Formation when samples are repeatedly analyzed. The
simultaneous linear expression of the residual compensation effect
and the regression analysis of the solutions to the Kissinger equation
for heating rate, yielded a kinetic parameter solution that correlates
with
T
max
. Furthermore, recalculated
T
max
values established a correlation between
the kinetic parameters,
T
max
, VR
o
, and BR
o
. The application of state-of-the-art numerical
correlations to measure subsurface kinetics, source rock richness,
and burial-depth temperatures will enhance the accuracy of reservoir
exploration and hydrocarbon production within the Bakken Formation.