An Integrated
Approach to Incorporate Intraplate Stress, Lithospheric Memory and Slip
Tendency Into Models for Fault
Zone Permeability
Worum, G.1,
J.D. Van Wees2, A. Gartrell3, F. Mulders2,
S.A.P.L. Cloetingh4 (1)
In the past decade, a variety of methodologies have been
developed for the characterization of fault
zone permeability. Analysis
techniques estimate
fault
permeability parameters from Shale Gauge Ratio (SGR)
and
fault
zone thickness. However, as recently shown for the
fault
transmissibility fails
to explain leakage. Here, a new fill-spill model has been produced for the Skua
Oil Field that challenges the importance of Mio-Pliocene
fault
reactivation as
the principal control on trap integrity. Integration of contemporary and
palaeo-fluid-flow indicators within a 3D structural framework, guided by 3D
structural restoration, highlighted the important role of pre-existing
fault
intersections. The
fault
reactivation can act as the principal control on
fault
permeability through the formation and opening of fractures in the
fault
zone.
Based on the insights
from this case study we developed an integrative model for qualititatively
assessing formation and opening of fractures, which take as input parameters:
(1) evolution of the stress field, (2) fault
slip tendency and
fault
displacement and (3)
fault
size, shape and linkage. It is demonstrated that the
integration of these factors can easily be incorporated in the standard
workflow of building 3D geological models for exploration and production.
Predicted
fault
fracture density magnitudes are qualitative and subject to many
uncertainties, which will be discussed. Of particular importance is knowledge
on the stress history and lithospheric memory (e.g. pre-existing
fault
size),
making particular
fault
zones more prone to
fault
reactivation and
fault
fracturization
than others.