Tectonothermal Evolution of the Apuseni Mountains, Romania: Resolution of Variscan versus Alpine Events with40Ar/39Ar Ages

Polyphase Alpine transcurrent faulting and thrusting in the Apuseni Mountains in Romania resulted in the juxtaposition of contrasting structural units that include both metamorphic assemblages and Permian‐Mesozoic cover. Resolution of the chronology of Alpine events and distinction from pre‐Alpine e...

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Veröffentlicht in:	The Journal of geology 1999-05, Vol.107 (3), p.329-352
Hauptverfasser:	Dallmeyer, R. D., Pană, D. I., Neubauer, F., Erdmer, P.
Format:	Artikel
Sprache:	eng
Schlagworte:	Argon Basement rocks Cooling Geological folding Geology Granite Muscovite Schist Shear zones Tectonics
Online-Zugang:	Volltext
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