The structural and kinematic development of the Austroalpine-Pennine boundary, S.E. Tauern, Eastern Alps

<p>The Eastern Alps are a belt of major deformation formed by the convergence and collision of Europe with the Adriatic microcontinent. A major tectonic boundary can be defined between the dominantly continental Austroalpine domain, which represents the northerly fringe of Adria; and the Penn...

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Bibliographic Details
Main Authors: Wallis, S, Wallis, Simon Richard
Other Authors: Platt, J
Format: Thesis
Language:English
Published: 1988
Subjects: