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A MINERAL BELONGING TO A GROUP OF COMPOUNDS FORMED BY SILICATES, PRESENT IN ERUPTIONAL ROCKS. FELDSPARS ARE ALUMININATED SILICATES OF ALCALINE METALS AND ALCALINE-EARTH. THEY ARE FORMING THE MOST IMPORTANT GROUP OF MINERALS PRESENT IN THE EARTH’S CRUST; BEING THE MAIN COMPONENTS OF MAGMATIC, SEDIMENTARY AND METAMORPHIC ROCKS.