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Structures and textures of MV-58A and quartz-mica schist MV-58C: (A) Pink gray and ocher saprolite of mica schists showing quartz venules along the schistosity; (B) Lepidoblastic layer of muscovite ...
While the source rock of aggregate B is an epidote-muscovite-plagioclase-alkali feldspar-biotite-quartz schist with a foliated structure and very fine lepidoblastic texture (crystals smaller than 1mm) ...
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The granitoids are classified as S-type hyperaluminous granites. This classification is supported by the presence of peraluminous minerals (e.g., muscovite) within the Iro granitoids, which also have ...
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