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

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...

Detaylı Bibliyografya
Asıl Yazarlar:	Peter Arkai, Peter Horvath, Geza Nagy
Materyal Türü:	Makale
Dil:	English
Baskı/Yayın Bilgisi:	Croatian Geological Survey 2010-11-01
Seri Bilgileri:	Geologia Croatica
Konular:	Gneiss Amphibolite Geothermobarometry Variscan regional metamorphism Tisza Unit Pannonian Basin Hungary
Online Erişim:	http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/266

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