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...

Cur síos iomlán

Sonraí bibleagrafaíochta
Príomhchruthaitheoirí:	Peter Arkai, Peter Horvath, Geza Nagy
Formáid:	Alt
Teanga:	English
Foilsithe / Cruthaithe:	Croatian Geological Survey 2010-11-01
Sraith:	Geologia Croatica
Ábhair:	Gneiss Amphibolite Geothermobarometry Variscan regional metamorphism Tisza Unit Pannonian Basin Hungary
Rochtain ar líne:	http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/266

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