Estimating displacement along the Brenner Fault and orogen-parallel extension in the Eastern Alps

The major structure accommodating orogen-parallel extension in the Eastern Alps is inferred to be the Brenner Fault, which forms the western boundary of the Tauern Window. The estimated amount of extension along this fault varies from a minimum of 10–20 km to a maximum of >70 km. All investigatio...

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Bibliographic Details
Published inInternational journal of earth sciences : Geologische Rundschau Vol. 100; no. 5; pp. 1129 - 1145
Main Authors Rosenberg, C. L., Garcia, S.
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer-Verlag 01.07.2011
Springer Nature B.V
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