An integrated palaeomagnetic and AMS study of the Tertiary flysch from the Outer Western Carpathians
The Carpathians belong to the European Alpine system, which was formed during the convergence and collision of the European and African plates. The study area, which comprises the Magura and Silesian nappes of the Outer Western Carpathians, were the locations of intensive folding and nappe transport...
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Veröffentlicht in: | Geophysical journal international 2009-06, Vol.177 (3), p.925-940 |
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Sprache: | eng |
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