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...
Main Authors: | , |
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Format: | Thesis |
Language: | English |
Published: |
1988
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