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紫金山铜金矿床发现的硫钼锡铜矿的分子式为Cu6.03Sn0.95Fe0.14Mo0.97S8.0,接近于理想的分子式Cu6SnMoS8,其与硫钨锡铜矿、硫铁锡铜矿一同出现在铜矿石中的现象是全球独有的。首次得出硫钼锡铜矿和硫钨锡铜矿的拉曼光谱位移主要出现在262、294、348、413、658、826 cm-1和256、291、345、430、654、860 cm-1等位置。这些含钨钼锡矿物组合的出现指示着强酸性、高氧逸度和高硫逸度的成矿环境,并预示深部的斑岩型矿床的存在。
The molybdenum-sulfur-molybdenum-tin-copper deposit found in the Zijinshan copper-gold deposit has a molecular formula of Cu6.03Sn0.95Fe0.14Mo0.97S8.0, which is close to the ideal molecular formula Cu6SnMoS8, which appears together with the sulfur-tungsten-tin-copper deposits and the iron- The phenomenon in copper ores is globally unique. For the first time, it was found that the Raman shift of the molybdenum-tin-copper and sulfur-tungsten-tin-copper deposits mainly occurs at 262,294,348,413,658,826 cm-1 and 256,291,345,430,654,860 cm- 1 and other locations. The presence of these tungsten-bearing molybdenum-tin mineral assemblages indicates strong acidogenicity, high oxygen fugacity and high sulfur fugacity of the ore-forming environment and indicates the presence of deep porphyry deposits.