5 46.65 0.84 52.98 100.47 5 13 Central Bar-3-1 45.8745.15 2.25 51.44 99.56 Southern Bar-6-5

5 46.65 0.84 52.98 100.47 5 13 Central Bar-3-1 45.8745.15 2.25 51.44 99.56 Southern Bar-6-5 four.35 50.62 100.12 six 14 Hanging Bar-4Bar-6-545.3244.76 1.12 52.38 98.82 Southern
five 46.65 0.84 52.98 one hundred.47 five 13 Central Bar-3-1 45.8745.15 2.25 51.44 99.56 Southern Bar-6-5 4.35 50.62 one hundred.12 six 14 Hanging Bar-4Bar-6-545.3244.76 1.12 52.38 98.82 Southern five.21 50.13 100.10 Northern Bar-5-146.1944.61 7.37 48.95 one hundred.93 7 15 Northern Bar-5-1 0.82 52.73 99.74 16 Northern Bar-5-1 44.65 six.09 48.61 99.35 17 Northern Bar-5-2 29.93 34.39 34.87 99.19 18 Northern Bar-5-2 30.21 33.96 34.82 98.99 19 Northern Bar-5-2 30.09 33.67 34.78 98.54 20 Northern Bar-5-2 30.03 33.91 34.61 98.55 21 Northern Bar-5-2 29.7 33.91 34.5 98.11 22 Rusty Bar-2-1 30.28 34.38 34.58 99.24 23 Rusty Bar-2-1 30.95 34.five 34.52 99.97 24 Rusty Bar-2-1 11.67 61.02 two.01 25.78 100.48 25 Rusty Bar-2-1 11.69 60.78 two.36 25.81 one hundred.64 26 Rusty Bar-2-1 11.98 55.46 7.35 25.66 100.45 27 Northern Bar-5-2 11.15 63.05 25.62 99.82 28 Northern Bar-5-2 11.18 62.90 25.19 99.deposit had been analyzed. The total Au-Ag strong answer are subdivided, according to Fe Cu Bi As S Total Formula [30] into AAPK-25 Cell Cycle/DNA Damage native gold–up to 30 atomic (at.) of Ag (PSB-603 manufacturer fineness 100000), electrum Bar-2-1 61.27 38.67 99.94 FeMineralogical (fineness 70000), “k telite” (mineral not approved by International 0.95 S1.05 Bar-2-1 60.73 39.ten 99.83 Fe0.94 S1.06 Association) with fineness 30000, and Au-containing silver (fineness 100).Fe1.00 (S1.92 As0.08 )2.00 Fe1.00 (S1.92 As0.08 )2.00 Fe1.00 (S1.96 As0.04 )2.00 Fe0.99 (S1.99 As0.02 )two.01 Formula Fe1.00 (S1.99 As0.01 )2.00 Fe0.95S 0.03 Fe1.00 (S1.97 As1.05 )two.00 Fe1.00 (S1.97 As1.06 )2.01 Fe0.94S 0.04 Fe1.00 (S1.96 As0.04 ))two.00 Fe1.00(S1.92As0.082.00 Fe0.99 (S1.94 As0.06 )two.00 Fe1.00(S1.92As0.08)two.00 Fe1.00 (S1.98 As0.01 )1.99 Fe1.00(S1.96As0.04 Fe0.99 (S1.94 As0.07 ))2.00 two.01 Fe0.99(S1.99As0.022.02 Fe0.99 (S1.93 As0.09 ))two.01 Fe0.99 (S1.89 As0.12 ))2.00 Fe1.00(S1.99As0.012.01 Fe1.00 (S1.90 As0.ten )two.00 Cu1.00 Fe0.99 S2.01 Cu0.99 Fe1.00 S2.01 Cu0.98 Fe1.00 S2.02 Cu0.99 Fe1.00 S2.01 Cu1.00 Fe0.99 S2.01 Cu1.00 Fe1.00 S2.00 Cu1.00 Fe1.02 S1.98 Cu4.84 Fe1.05 Bi0.05 S4.06 Cu4.83 Fe1.06 Bi0.06 S4.06 Cu4.54 Fe1.12 Bi0.18 S4.16 Cu4.98 Fe1.00 S4.01 Cu5.01 Fe1.01 S3.Note: 1–Pyrrhotite FeS; 36–Pyrite FeS2 ; 173–Chalcopyrite CuFeS2 ; 248–Bornite Cu5 FeS4 .Minerals 2021, 11,7 ofTwo hundred grains of gold from diverse zones and places from the Baranyevskoe deposit were analyzed. The full Au-Ag strong answer are subdivided, in accordance with [30] into native gold–up to 30 atomic (at.) of Ag (fineness 100000 ), electrum (fineness 70000 ), “k telite” (mineral not approved by International Mineralogical Association) with fineness 30000 , and Au-containing silver (fineness 100 ). The composition in non-oxidized samples varies from low-grade to high-grade gold with a gap in the isomorphic series inside the selection of Au 748 at. . Some gold grains from the Rusty and Central zones, the majority of the grains in the Hanging zone and half with the gold grains from the Northern zone consist of native gold and electrum having a array of fineness of 52138 (Figure 6, based on data in Table 2), that are characteristic of the gold-pyrite-quartz association of the early ore-forming stage. A significant part of gold grains from the Northern zone and a few grains from the Hanging zone correspond to high-grade native gold (88341 ) (Figure six, determined by data in Table 2), standard on the gold-sulfosalt-quartz association. Electrum, “k telite”, along with the high-grade native gold are representative inside the Southern zone from sediments under of quartz veins and in oxidized ores. Oxidized ores of Southern and Central zones.