Photography: Hossein Barkhordari via imaggeo.egu.eu.
Geology & Geophysics
Worldwide

Fault-valve behaviour of petroleum traps

Along-fault fluid flow at a critical segment of a fault can eloquently explain the initial reservoir pressure and hydrocarbon column height in a fault-bound trap. Episodic fluid expulsion at this fault-valve, therefore, provides a dynamic addition to a traditional view that fault-bound traps are only controlled by across-fault fluid flow

When evaluating fault-bound traps, it is common practice to map around-the-fault pathways through diligent seismic interpretation, juxtaposition diagrams, and 3D structural framework construc­tion. It is also common practice to ad­dress across-fault sealing and evaluate hydrocarbon column heights by using industry-standard clay-smear algorithm correlations. Yet, quantifying along-fault hydraulic conductivity through fault-reactivation pressure is rare in trap evaluation, despite faults being consid­ered as migratory pathways.

Fault reactivation pressures are calculated using the critically stressed fault concept related to shear failure. This geomechanical concept was ap­plied in a study on an underfilled fault-bound oil field off the coast of Sabah, offshore Malaysia. The prima­ry fault extends near the seabed, and the quality of seismic imaging above the crest of the trap is diminished. This reduction in image quality is in­terpreted as indicative of a gas cloud. The study identified a connection be­tween the initial reservoir pressure, the hydrocarbon column height, and the fault reactivation pressure on a critical segment of the fault near the crest of the trap. Furthermore, the fault reacti­vation pressure is lower than the mini­mum horizontal stress.

It is hypothesized that an increase in reservoir pressure at the critical fault segment can trigger fluid flow along the fault and out of the trap. The cycli­cal nature of this dynamic behaviour is referred to as fault-valve after Sibson’s original model published in 1990. In an active petroleum system, it forms a credible way to explain fluid release from a trap in addition to the other pathways mentioned above.

Recognizing that along-fault flu­id flow can control the hydrocarbon column in a trap is not new. Howev­er, applying the critically stressed fault concept to evaluate fault-bound traps is rarely done. Reasons for this may be that the concept is not appreciated by all geoscientists. Also, many integrated subsurface software packages do not carry a fault reactivation module in their fault interpretation or structur­al framework section. Lastly, there is significant uncertainty associated with fault strength parameters, which may be considered too wide to yield mean­ingful results.

The critically stressed fault concept and its related fault-valve model are considered viable trapping mechanisms, impacting existing exploration, apprais­al and production projects. This is par­ticularly relevant when recognizing that preferentially oriented faults have the potential to leak at fluid pressures below the minimum horizontal stress.

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