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萤石矿化现象广泛分布在吉尔吉斯境内,并与汞-锑矿床、锡矿床、钨矿床、多金属矿床及其它矿床一起决定了吉尔吉斯的成矿特点。氟化物在成矿作用中起着促进元素呈SiF_6~(2-)、BF_4~-、[Su(F,OH)_6]~(2-)、以及钨、铌、钽、稀土的含氟氧化物型络合物形式迁移的重要矿化剂作用。氟主要呈萤石形式沉淀下来,加入由壳源花岗岩类岩浆作用形成的锡矿床、稀土矿床和其它一些矿床的矿石组份。氟作为流体的组份,在发生于地幔条件下的超基性岩浆
Fluorite mineralization is widely distributed in Kyrgyzstan and, together with the mercury-antimony deposits, tin deposits, tungsten deposits, polymetallic deposits and other deposits, determine the metallogenic characteristics of Kyrgyzstan. Fluoride plays a key role in the metallogenesis of SiF_6 ~ (2 -), BF_4 ~ -, [Su (F, OH) _6] ~ (2-), and the fluoridation of tungsten, niobium, tantalum and rare earth Important Mineralizer Effect of Form Complex Migration. Fluoride mainly precipitated in the form of fluorite, adding tin ore, rare earth deposits and other ore components formed by crust-derived granitic magmatism. Fluorine is used as a fluid component in ultramafic magmas that occur in mantle conditions