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...
| Egile Nagusiak: | , , |
|---|---|
| Formatua: | Artikulua |
| Hizkuntza: | English |
| Argitaratua: |
Croatian Geological Survey
2010-11-01
|
| Saila: | Geologia Croatica |
| Gaiak: | |
| Sarrera elektronikoa: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/266 |