Hi all,
I am studying a coarse grained staurolite-garnet-sillimenite (fibrolitic) bearing quartzo-feldspathic schist (quartz-feldspar-biotite-muscovite-garnet-staurolite-sillimenite) from a deformed and metamorphosed Precambrian terrain. Previous authors have described them as pelitic schists. However, these schists have nearly 10-12 modal% feldspar indicating they are not pelites.
The feldspar grains are extremely coarse and subhedral (not rounded) like those from deformed igneous rocks (photomicrographs attached). I have a suspicion that they may not be detrital and the original rock was a granite (peraluminous) rather than a quartzo-feldspathic sediment. Is there any way to identify its possible source from the whole rock analysis of this rock or from any other aspect? The original texture and mineral assemblage is partially modified due to deformation and metamorphism.
Feldspar compositions vary roughly between Ab70An30 to Ab60An40 (Or component is 0.1-0.3).