Sample 82MW0015 is a fine-grained orthogneiss
composed of plagioclase (35%), K-feldspar (30%), quartz (30%), biotite
(4%), and trace muscovite, oxides, and sphene. Relatively small
plagioclase porphyroclasts reach 3.5 mm. Alteration and
recrystallization is extreme in seritized K-feldspar. Relict 8 mm-long
K-feldspar porphyroclasts have totally recrystallized, but are still
wrapped by biotite. A foliation is defined by micas and banding of
felsic minerals. |