“…Source apportionment studies focused on the long-distance transport of aerosols have effectively used MRS. A study over Kozani, Northern Greece [85] showed the existence of various mineral phases in the collected aerosols, such as calcite (1084, 710, 274, and 149 cm −1 ), gypsum (1134, 1006, and 413 cm −1 ), titanium oxide (627, 390, and 148 cm −1 ), feldspar (510, 474,285, 265, 150, and 109 cm −1 ), lepidolite (1573, 1347, 728, 382, and 288 cm −1 ), and smectite (1379, 731, 385, 288, and 141 cm −1 ). The presence of lepidolite (mica) and smectite (clay) was associated with the long-distance transport of Saharan dust.…”