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...

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Bibliographic Details
Main Authors: Gyorgy Buda, Elemér Pál-Molnár, Friedrich Koller
Format: Article
Language:English
Published: Croatian Geological Survey 2012-06-01
Series:Geologia Croatica
Subjects:
Online Access:http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/550

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