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- W4385990803 abstract "Summary A large cross-disciplinary research project funded by a mining company in the Galilee Basin (Queensland) was undertaken from August 2020 to December 2021. This project involved six individual researchers / practitioners with expertise in geology, geophysics, structural geology, hydrogeology and geomechanics. The purpose of the project was to investigate the potential for vertical transfer of groundwater through the Rewan Formation (regarded as a regional aquitard) via preferential flow paths within faults, fractures or connected lithological units. Using multiple lines of evidence from different disciplines, the project was able to determine that: (a) the critical deformation mechanism within Triassic sedimentation is layer parallel shear with no need to invoke significant faulting; (b) there are no faults with demonstrable displacement; (c) the juxtaposition of lithologies across a fault plane is overwhelmingly self-juxtaposition; (d) a complete breach of the Rewan Formation by a fault is impossible; (e) on acoustic scans, there are only rare occurrences of discontinuities that could be potential conduits with enhanced flow; (f) acoustic scans show no lateral continuity of fractures between holes only 30 m apart; (g) in situ fractures will be generally compressible and mechanically weak due to relatively low elastic moduli; (h) geochemical analysis confirms that ecologically important springs have a shallow source (above the Rewan Formation); and (i) the Rewan Formation is confirmed to be dominantly argillaceous." @default.
- W4385990803 created "2023-08-19" @default.
- W4385990803 creator A5085289313 @default.
- W4385990803 date "2023-01-01" @default.
- W4385990803 modified "2023-10-14" @default.
- W4385990803 title "Fault Zone and Hydraulic Connectivity Analysis - Rewan Formation, Galilee Basin, Queensland" @default.
- W4385990803 doi "https://doi.org/10.3997/2214-4609.202373010" @default.
- W4385990803 hasPublicationYear "2023" @default.
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