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...
| المؤلفون الرئيسيون: | , , |
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| التنسيق: | مقال |
| اللغة: | English |
| منشور في: |
Croatian Geological Survey
2010-11-01
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| سلاسل: | Geologia Croatica |
| الموضوعات: | |
| الوصول للمادة أونلاين: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/266 |