“…For the purpose of the present study, each carbonate rock type was grouped by five selective hand specimen samples. They consist of dark gray limestones (samples B20, B28, B33, B45, and B49), light gray limestones (samples B1, B26, B32, B36, and B41) and dolomitic limestones (samples F17, F18, F20, F23, and F26) ( Figure 2 wavelength region centered at 2.530-2.541 μm and 2.333-2.340 μm and 2.503-2.520 μm and 2.312-2.323 μm, respectively [39,41,[45][46][47][48][49], due to the vibrational processes of carbonate ions CO [39,41,46]. The presence of clay and other phyllosilicate minerals in an intimate mixture with carbonates can be identified based on their vibrational absorption features around 2.20 μm and 2.30 μm [40][41][42].…”