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钾长石化是斑岩铜(钼)矿床的一种重要蚀变,也是找矿评价标志之一。本文提供了高温高压实验研究富家坞斑岩铜(钼)矿床钾长石化条件的初步结果,以期对进一步研究该类矿床成因机理和指导找矿评价有所邦助。一实验条件的确定实验在体积为10~13毫升的自紧式高压釜中进行。实验条件是根据矿床地质特征和包果体资料确定的。
Potash feldspathization is an important alteration of the porphyry copper (molybdenum) deposit and is also one of the signs of prospecting evaluation. This paper provides preliminary results of high-temperature and high-pressure experiments on the potash feldspathization of the Fujiatang porphyry copper (molybdenum) deposit, in the hope of helping to further study the genesis mechanism of this type of deposit and to guide ore prospecting. A determination of the experimental conditions Experiments in a volume of 10 to 13 ml autofrettage autoclave. The experimental conditions are based on the geological characteristics of the deposit and the package fruit body data to determine.