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    Enclaves in the S-type granites of the Kösseine massif (Fichtelgebirge, Germany): implications for the origin of granites

     The Hercynian peraluminous granites of the Kösseine massif differ in composition and content of enclaves from the other granites of the Fichtelgebirge. They are garnet-, cordierite- and andalusite-bearing S-t...

    S. Schödlbauer, L. Hecht, A. Höhndorf, G. Morteani in Geologische Rundschau (1997)