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Porphyry-type molybdenum deposits in the eastern Qinling Mo belt, central China

机译:中国中部秦岭钼矿带斑岩型钼矿床

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摘要

The Eastern Qinling mineralizing belt of porphyry-type Mo deposits is located in the south margin of North China Platform. About 40 /100 explored Mo resources of China are stored in that belt. Mo mineralization is Related with Yanshanian (161-104 Ma) small intermediate to acidic porphyry bodies. As the porphyry Bodies intruded into Archean to middle Proterozoic carbonate rocks and alumino-silicate rocks, Porphyri-type, skarn-type and hornfels-type Mo ores were formed with different types of wallrock Alteration. Ore-forming fluids are characterized by H_2O-CO_2-NaCl with lower to middle saline (0-12.7 /100 NaCl).
机译:东秦岭斑岩型钼矿床成矿带位于华北台地南缘。中国约有40/100的探明钼资源储藏在该带中。钼矿化与酸性斑岩体中的小燕山期(161-104 Ma)有关。随着斑岩体侵入太古代至中元古代的碳酸盐岩和铝硅酸盐岩,形成了斑岩型,矽卡恩型和角铁型的矿石,并形成了不同类型的围岩蚀变。成矿流体的特征在于H_2O-CO_2-NaCl的盐浓度较低至中等(0-12.7 / 100 NaCl)。

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