斑岩型铜(金)矿床成矿元素大规模堆积制约机制研究

来源 :矿物学报 | 被引量 : 0次 | 上传用户:yanlian2008
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斑岩型矿床规模大,易开采,是Cu、Mo最主要类型矿床,亦是Au的重要类型矿床(Halter等,2002),因而近数十年来斑岩型铜(金)矿床一直是矿床学研究热点课题之一。研究结果表明,斑岩铜(金)矿床与与高氧逸度岩浆岩具有紧密的共生关系。这和铜、金及硫等元系在岩浆中的地球化学行为有关 Porphyry type deposits are large and easy to be exploited. They are the most important types of deposits of Cu and Mo and are also important Au deposits (Halter et al., 2002). Therefore, the porphyry copper (Au) deposit has been a mineral deposit for decades One of the hot topics. The results show that the porphyry copper (Au) deposit has close symbiosis with high magmatic oxygen and magmatic rocks. This is related to the geochemical behavior of elements such as copper, gold and sulfur in magmas
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