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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Published in | International journal of earth sciences : Geologische Rundschau Vol. 100; no. 5; pp. 1129 - 1145 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Berlin/Heidelberg
Springer-Verlag
01.07.2011
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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