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Top Seal and Compartmentalisation in the Kingia Play, implications for porosity preserving Plays.
Presented by Alex Fuerst (Molyneux Advisors)
In the Kingia play of the North Perth Basin, significant compartmentalisation is observed across the basin and within individual fields, despite the sand-on-sand juxtaposition. This compartmentalisation manifests in both pressure and phase (gas/water) variations. Cemented fractures are observed near fault zones in Perth Basin wells. This results in decreased permeability near faults, as evidenced by local wells in the Perth Basin.
SEM images show fractures within grains of grain coated sands are sufficient to serve as nucleation sites for quartz cementation. In contrast, within the Irwin River Coal Measures (IRCM), the grain surfaces alone provide sufficient sites for cementation. The IRCM sands exhibit permeabilities that are characteristic of seals, with samples displaying quartz cementation, kaolin cementation, or a combination of both.
The implications for play risk / play maps are significant. Shallower Kingia penetrations face an unproven top seal due to the less cemented IRCM, potentially explaining the multiple shallower exploration failures. At greater depths, the presence of more complex faulting may enhance fault seal integrity and lead to more intricate trap configurations. However, this also likely increases development complexity due to reservoir compartmentalization. The observed improvement in IRCM sealing capacity with depth suggests broader implications for exploring deeper grain-coated plays, allowing for a wider range of facies to be considered as potential seals.
Timings for the event:
Date: Thursday 21st November, 2024
Venue: The Shoe Bar, Yaga Square, Perth
Time: 6pm – 8pm (Perth time)
PESA Members: $25.00 (PESA Members must Log on to the PESA website to purchase)
Non-members: $50.00
PESA Students Members: Free (registration is essential)