Research Article

Mineralogy, Geochemistry, and Origin of Buyukmahal Manganese Mineralization in the Artova Ophiolitic Complex, Yozgat, Turkey

Table 4

Composition of pyrolusite (pr) samples of Buyukmahal ore.
(a)

Si Ti Al Fe Mn Mg Ca Na K Ba Ag Zn

pr482.610.080.613.2675.710.090.600.000.050.250.000.00
pr492.260.100.432.7080.480.040.550.060.050.950.010.06
pr501.520.190.423.0074.900.080.490.030.090.200.020.06
pr512.320.080.593.0276.440.060.400.050.160.320.020.00

Ave.2.180.110.512.9976.880.070.510.030.090.430.010.03

(b)

SiO2TiO2Al2O3Fe2O3MnOMgOCaONa2OK2OBaOAg2OZnO

pr485.580.131.154.6697.760.150.080.000.060.280.000.00
pr494.830.170.813.86103.920.070.770.080.061.060.010.07
pr503.250.320.794.2996.710.130.690.040.110.220.020.07
pr514.960.131.114.3298.700.100.560.070.190.360.020.00

(c)

Number of ions calculated on the basis of 2 (O)
Coef.SiTiAlFeMnMgCaNaKTotal

pr481.200.110.000.030.081.650.000.000.000.001.87
pr491.160.090.000.020.061.700.000.020.000.001.90
pr501.270.070.010.020.081.730.000.020.000.001.92
pr511.200.100.000.030.071.670.000.010.000.001.89

Ave.1.210.090.000.020.071.690.000.010.000.001.90