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- W2186625153 abstract "For the Brenner Normal Fault (BNF), a ductile and brittle history has to be considered. The ductile part of the BNF is a low-angle, W- dipping mylonite zone which compensated the exhumation of the western Tauern Window during Neogene convergence between the Adriatic and European plates. In addition, the contact between the foot- and hangingwall blocks is marked by a discrete brittle fault which dips moderately to W. The area W of the BNF surface trace and south of the Upper Inn Valley is seismically characterized by low magnitude events. Earthquake epicentres are scattered in a broad zone which extends up to 15 km west of the BNF. Hypocenter depths range between 5 and 18 km. The density of epicentres continuously decreases towards W while the depth of hypocenters increases. Focal plane solutions can be separated into three categories: (1) Strike-slip earthquakes (NE or NW striking faults) indicating N-S shortening; (2) A second group of solutions proves E-W extension, possibly at the BNF; (3) A third group of events was produced by thrust faults, indicating N-S-shortening at different crustal levels. Preliminary data of permanent GPS stations located on both sides of the BNF and in the north Alpine foreland indicate N/NW directed movement of the Alpine stations relative to the foreland in the order of ~1 mm/yr and E-W extension across the BNF in the order of ~0.5 mm/yr. As a model for active crustal movements we suggest (1) N(NW)-directed thrusting of the central Alpine nappe stack and (2) contemporaneous E-W extension which uses the weakness zone of the BNF." @default.
- W2186625153 created "2016-06-24" @default.
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- W2186625153 date "2005-01-01" @default.
- W2186625153 modified "2023-09-27" @default.
- W2186625153 title "Indications for activity of the Brenner Normal Fault zone (Tyrol, Austria) from seismological and GPS data" @default.
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