Global Journal of Science Frontier Research, G: Bio-Tech & Genetics, Volume 22 Issue 2

Figure 3: The marble specimen under petrographic microscope,(i) Marble PPL and (j)Marble XPLfrom C5.1 sample ii. Geochemical result The purpose of geochemical analysis is to identify the constituents of Khewa Calcite Marble's chemical makeup. The XRF analysis results in the determination of 28 elements. The elements with the highest percentages are silicon, calcium, magnesium, aluminum, iron, potassium, and sulfur, as well as heavy metals like Fe, Cr, and Ti. Table 1: Shows the oxide percentage in Marble in its adjacent rocks with PPM Oxides C1-1 C2-2 C3-3 C4-4 C5-5 Over all PPM MgO 124169.281 129315.227 118810.945 40573.023 41836.957 454705.433 AI 2 0 3 9800.377 6439.447 40826.293 164967.313 163134.250 385167.680 Si0 2 15316.664 11887.871 13935.673 758900.938 90381.525 890422.671 Fe 2 0 3 385.620 409.443 2564.272 60375.730 52280.992 116016.057 Cr 2 0 3 101.027 45.940 166.520 254.507 172.603 740.597 CaO 43167.294 41281.397 35411.609 27817.947 24670.201 172348.448 TiO 2 0.000 0.000 762.605 6597.444 6378.446 13738.495 K 2 0 521.857 382.843 3485.495 32264.771 27118.930 63773.896 S0 3 2145.588 2357.083 7541.333 8220.825 4054.696 24319.525 P 2 0 5 0.000 0.000 0.000 2745.132 3472.462 6217.594 Figure 4: The graph shows the high point of SiO 2 © 2022 Global Journals 1 Year 2022 98 Global Journal of Science Frontier Research Volume XXII Issue ersion I VII ( G ) Petrological, Geochemical and Mechanical Characteristics of Kooz Kunarr Khewa Calcite Marble (i) (j)