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在花岗岩浆侵入活动过程中,于岩浆期后气热溶液交代作用阶段,往往伴有某些稀有元素的矿化现象。如铍的矿化已经许多资料说明,概与钠长石化和云英岩化等交代作用具有密切关系。据 A.A.别乌斯等阐述铍在高温气热溶液中的存在形式,极大可能是与氟合成络离子([BeF_1]~(2-))进行运移。关于铍的沉淀矿化作用,以往资料多认为是介质的
During granite magma intrusion, during the stage of metasomatic replacement of gas-hot solution after magmatic stage, mineralization of some rare elements often accompanies. Mineralization of beryllium, for example, has been described by many sources and is closely related to the explanation of albite and dolomitization. According to A.A. Bauhin, et al., The existence of beryllium in high-temperature gas-heat solution is highly probable that it is transported with fluorine complex ion ([BeF_1] ~ (2-)). On the mineralization of beryllium precipitation, the past data and more think is the medium