Calderitic garnet and manganoan deerite have been found in Al-poor, Fe-Mn-rich quartzites associated with metabasic schists on the island of Andros, Cycladic blueschist belt, Greece. Calderitic garnet (30-45 mole ~ calderite, 55-70 mole ~ andradite, 0-2 mole ~ spessartine) occurs in paragenesis with quartz, rhodonite, rhodochrosite, Ni-Mn-bearing magnetite (2-20 mole ~ trevorite, 6-12 mole ~ jacobsite, 73-91 mole ~ Fe304) , baryte, and orthite. Deerite is associated with quartz, garnet (rich in spessartine, almandine, and andradite), phengite, aegirine, magnetite (containing up to 12 mole ~o jacobsite), and crossite/riebeckite. Deerite contains 33.0-34.4 wt. ~ SiO2, 0.53-5.5 wt. ~ TiO 2, 0.09-0.31 wt. ~ A1203, 11.9-33.9 wt. ~ MnO, 17.5-44.2 wt. ~ FeOtot, and 1.5-2.8 wt. ~ MgO. MnO contents correspond to 29-77 cation ~ Mn 1+ per total R 2+ cations. Deerites from Andros are thus closer to the hypotheticat end-member mangano-deerite, 2 + 3 + 9 Mn12 Fe6 $112040(OH)10, than any other analysis of deerite so far published.