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建立深成岩与火山岩研究之间的有机联系,对于理解从火山喷发到岩浆-热液矿床形成的各种岩浆过程是非常必要的。斑岩铜矿床普遍与规模较大且长期活动的火山中心有密切联系,但是关于矿化侵入体与火山喷发的时间和动力学机制方面的联系仍存在很大的争议。
Establishing an organic link between deep diagenesis and volcanic rock research is necessary to understand the various magmatic processes from volcanic eruption to magmatic-hydrothermal deposits. Porphyry copper deposits are generally associated with large-scale and long-term volcanic centers, but there is still considerable controversy over the timing and kinetic mechanisms of mineralized intrusions and volcanic eruptions.