EGU21-12238
https://doi.org/10.5194/egusphere-egu21-12238
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Partitioned Permeability Diagram: an innovative way to estimate Fault Zones hydraulics.

Irène Aubert, Juliette Lamarche, and Philippe Leonide
Irène Aubert et al.
  • Cerege, Aix-Marseille Université, Marseille, France

Understanding the impact of fault zones on reservoir trap properties is a major challenge for a variety of geological ressources applications. Fault zones in cohesive rocks are complex structures, composed of 3 components: rock matrix, damage zone fractures and fault core rock. Despite the diversity of existing methods to estimate fault zone permeability/drain properties, up to date none of them integrate simultaneously the 3 components of fracture, fault core and matrix permeability, neither their evolution with time. We present a ternary plot that characterizes the fault zones permeability as well as their drainage properties. The ternary plot aims at (i) characterizing the fault zone permeability between the three vertices of matrix, fractures and fault core permeability ; and at (ii) defining the drain properties among 4 possible hydraulic system: (I) good horizontal and vertical, fault-perpendicular and -parallel; (II) moderate parallel fluid pathway; (III) good parallel fault-core and (IV) good parallel fractures. The ternary plot method is valid for 3 and 2 components fault zones. The application to the Castellas Fault case study show the simplicity and efficiency of the plot for studying underground and/or fossil, simple or polyphase faults in reservoirs with complete or limited permeability data.

How to cite: Aubert, I., Lamarche, J., and Leonide, P.: Partitioned Permeability Diagram: an innovative way to estimate Fault Zones hydraulics., EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-12238, https://doi.org/10.5194/egusphere-egu21-12238, 2021.

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