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- W146937249 abstract "Geological and hydrogeological field evidence from several sites (Grimsel Test Site, Äspö Hard Rock Laboratory, deep boreholes in northern Switzerland, various mines) shows that in spite of contrasting geological settings, evolutions and ages, several common characteristics of water-conducting features exist in crystalline basement rocks. Geometric and hydraulic properties of water-conducting features depend mainly on the mechanism of brittle deformation (e.g. faulting, jointing), on the nature and intensity of water/rock interactions (e.g. hydrothermal fracture sealing) and on rock type. Leucocratic rocks, such as aplite/pegmatite dykes, have higher fracture frequencies and transmissivities when compared to more basic rocks. Brittle deformation in most crystalline-rock environments occurred recurrently, and pre-existing structures (e.g. lithologic contacts, ductile shear-zones, older fault and fracture generations) were preferentially reactivated. Faults of different sizes, ranging from small cataclastic zones to regional lineaments, are the most important structures in which flow occurs. Due to the complex architecture of faults in directions parallel and perpendicular to strike, the spatial distribution of flow in faults is very heterogeneous. Hydrothermal alteration events lead to fracture scaling by mineral precipitation or to increased apertures due to the dissolution of pre-existing fracture infills, thereby enhancing the heterogeneity of the flowpaths on a small scale." @default.
- W146937249 created "2016-06-24" @default.
- W146937249 creator A5030929731 @default.
- W146937249 date "2000-01-01" @default.
- W146937249 modified "2023-10-14" @default.
- W146937249 title "Geological and Hydraulic Properties of Water-Conducting Features in Crystalline Rocks" @default.
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- W146937249 doi "https://doi.org/10.1007/978-94-017-1816-5_1" @default.
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