The δ30Si-δ18O results suggest that quartzes are magmatic hydrothermal in origin. The δ18O-δ13C isotope results show that carbon of skarn and magnetite marble related with mineralization was mainly from mantle,except that partial carbon resulted from solution of marine carbonate.
δ30Si、δ18O的研究结果表明,石英主要为岩浆热液成因,δ13C、δ18O同位素的研究结果表明,与成矿有关的矽卡岩、磁铁矿大理岩中的碳除部分来源于海相碳酸盐岩的溶解外,主要来源于地幔,多不杂矿区的硫同位素研究结果表明成矿物质主要来自岩浆流体。
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Finally, skarn and ores show typical textures and structures of magmatic deposits.
矿石、矽卡岩具有典型的岩浆矿床的结构构造。
The Tongshan skarn type copper deposit in Guichi county has well-developed garnet skarn zone.
研究区为矽卡岩铜矿床,岩体与围岩接触带石榴石矽卡岩十分发育。
The contact deposit is controlled by the contact zone, and shows typical features of skarn orebody.
接触带矿体受接触带控制,具矽卡岩型矿体典型特征。
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