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- W1566013329 abstract "Abstract Calcite veins in a limestone-shale succession in SW England were formed by geothermal water and injected along normal faults. Vein length/thickness ratios indicate that their fluid overpressure was 20 MPa, suggesting a depth to the fluid sources beneath the present exposures of several hundred metres. Many subvertical veins are restricted to limestone layers, reducing the temporary permeability. When hydrofracture fluid overpressure is the only loading, soft layers tend to arrest hydrofractures, whereas stiff layers favour their propagation. Veins dissecting many layers form subvertical extension fractures in the limestone layers but thinner inclined shear fractures in the shale layers. Vein aperture changes between layers suggest that flow channelling may be important in layered reservoirs." @default.
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- W1566013329 date "2004-01-01" @default.
- W1566013329 modified "2023-09-26" @default.
- W1566013329 title "Permeability in Layered Reservoirs: Field Examples and Models on the Effects of Hydrofracture Propagation" @default.
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- W1566013329 doi "https://doi.org/10.1016/s1571-9960(04)80112-5" @default.
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