A foliated amphibolite, sample 81MW0005 is
comprised of plagioclase (35%), hornblende (20%), biotite (20%), epidote
(15%), quartz (9%), and trace oxides and sphene. Plagioclase is mostly
fine grained and subhedral and occurs in the matrix. Fine-grained
hornblende occurs as anhedral pleochroic green-tan crystals. Biotite is
partly, but not entirely aligned in the foliation, suggesting that
deformation took place before a secondary growth of biotite. Epidote is
anhedral, and sometimes rimmed by biotite. Quartz occurs in 2 mm-thick
aggregates and shows subgrain development. |