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A segment of the Salzach-Ennstal fault zone (Talhof fault, Eastern Alps) shows evidence for joint nucleation by layer-parallel shear, causing the formation of joint-bounded slices oriented at high angles (65–85°) with respect to the shear zone boundary (SZB). Subsequent slice rotation resulted in joint reactivation as antithetic shears, slice kinking, and breaking-up of the individual slices into...
Die hydrogeologische Beurteilung von Gebirgskörpern wird maßgeblich von Störungszonen beeinflusst, die als Wasserleiter, Barrieren oder einer Kombination von beiden auftreten. Der heterogene, strukturell komplexe Aufbau ergibt richtungsabhängige hydraulische Eigenschaften innerhalb der Störungszonen und ihrer strukturellen Einheiten (Domänen). An der Talhof-Störung (Semmering-Raxgebiet, Österreich)...
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