Fault
Facies Modeling: Applications in Various Sedimentary and
Fault
System Configurations
Muhammad Fachri, Jan Tveranger, Nestor Cardozo, and Sylvie Schueller
Centre for Integrated Petroleum Research, University of Bergen, Bergen, Norway
Fault
facies modeling is the process of generating 3D geological objects in the
fault
envelope in reservoir grid. The modeling is performed to capture reservoir heterogeneity caused by faulting. The conditioning factors for
fault
facies modeling are a
fault
product distribution factor (FPDF, a parameter describing the distribution of lithologies in the
fault
envelope) and a shear strain parameter.
FPDF is generated based on the following variables:
1. Pre-faulting sedimentary facies configuration in the fault
envelope
2. Fault
displacement model, which is constrained based on the following input variables:
- fault
core thickness as a function of
fault
throw
- footwall and hanging wall damage zone widhts as functions of fault
throw
- the displacement percentage accommodated by fault
core and damage zones
- the type of displacement function
The strain parameter is generated based on the fault
displacement model. The strain parameter, together with the FPDF, is used for creating the probability distribution that serves as an input in stochastic modeling of the
fault
facies. The
fault
facies volumetric proportion and spatial distribution in the resulting models can be partly controlled by applying simple manipulations to the
fault
facies probability distribution.
The modeling technique allowed many synthetic fault
envelope models to be built easily by varying the modeling input variables constrained by field data. The resulting models were systematized in matrix form, capturing the variation of both sedimentary and
fault
system configurations. Currently 64 models have been implemented, each executed in 10 stochastic realizations. Quantitative analysis of the implemented models shows that the application of the modeling technique is able to reproduce natural
fault
envelope configurations formed under various sedimentary and structural configurations.
AAPG Search and Discovery Article #90078©2008 AAPG Annual Convention, San Antonio, Texas