“…These crystals present pleochroism [2,3] and commonly appear in metamorphic pelitic sediments. It is generally a crystal available only as a mineral although some very small specimens have been grown in the laboratory [4]. A variety of experimental studies have been devoted to the determination of the crystal structure [5][6][7], nuclear magnetic resonance [8,9], EPR [10,11], optical absorption [2,12,13] and other properties of this mineral [14,15].…”