A Clockwise P-T Path from the Variscan Basement of the Tisza Unit, Pannonian Basin, Hungary

<div>The polymetamorphic basement of the Tisza Unit forms a detached</div><div>fragment of the Variscan European foreland of the Neotethyan</div><div>realm. A clockwise evolution path of a gneiss-amphibolite complex</div><div>of the Tisza Unit was reconstruc...

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Bibliografiska uppgifter
Huvudupphovsmän: Peter Arkai, Peter Horvath, Geza Nagy
Materialtyp: Artigo
Språk:Inglês
Publicerad: Croatian Geological Survey 2010-11-01
Serie:Geologia Croatica
Ämnen:
Gneiss
Amphibolite
Geothermobarometry
Variscan regional metamorphism
Tisza Unit
Pannonian Basin
Hungary
Länkar:http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/266
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