“…Feldspars are natural aluminosilicates, constituting one of the largest groups of minerals found in the Earth's crust [7]. In alkaline-earth feldspars MAl 2 Si 2 O 8 (M=Ca, Sr, and Ba), its structures are constructed by an array of interlinked corner-sharing SiO 4 It is known that Eu 3+ ions are good luminescent centers for many red phosphors due to their excellent red-emission [11,12].…”