Biotite replacing garnet, from the Willoughby area of the Vermont Appalachians.
#ThinSectionThursday π₯ Hot off the microscope this morning! π€ This may look dull, but the big clear (grey) grain with faint WSW-ENE parallel lines, on the right hand side of the image is a shocked quartz (produced by a meteorite impact).
The smaller greenish (orange) grain to the left is epidote. All the fragmental grains here been cemented together by turbid brown albite. From the enigmatic Stac Fada unit, (Proterozoic), in NW Scotland.
Titanite encircling illmenite in an amphibolite-facies metabasalt.
Perthite, in a fayalite-hastingsite hypersolvus granite, Cauro-Bastelica Complex, Tolla dam, Corsica
The minerals crystallized from melt at high temperature and water-poor conditions.