Mafic enclaves in peraluminous Variscan granitoid in the Battonya Unit from Southeast Hungary
<p>Variscan granitoids occur in the southeastern part of the Tisza Mega Unit of Hungary. The presence of amphibole, calc-alkaline-type Mg-rich biotite in metaluminous basic enclaves, and muscovite and Fe-Al-biotite in peraluminous granitoids, suggests a mixed I-S-type origin. Two types of musc...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Croatian Geological Survey
2012-06-01
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Series: | Geologia Croatica |
Subjects: | |
Online Access: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/550 |