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红格钒钛磁铁矿区共生的碱性岩脉型铌钽矿床,经多年来的地质工作初步查明属霓石花岗伟晶岩铌锰矿——褐钇铌矿——锆英石型和霓石钠铁闪石正长伟晶岩、钠长岩烧绿石——锆英石型矿脉。稀有矿脉在空间分布上与含钒钛磁铁矿层状基性——超基性岩体的上部矿层密切共生。已经初勘的路枯矿段主要矿脉的铌钽储量达中型以上,且红格
Alkali-veined niobium-tantalum ore deposits symbiotic with the Hongge vanadium-titanium magnetite deposit have been initially identified as gem-niobite-pegmatite niobium-manganese ore-brown yttrium niobium ore-zirconite and aegirine by years of geological work Sodium iron amphibole is a long pegmatite, albite pyrochlore - zircon-type veins. Rare mineral veins are closely related to the upper ore bed of the base-ultrabasic rock mass containing vanadium-titanium magnetite in spatial distribution. The primary mineral vein of the Lukuang section, which has been initially explored, contains more niobium and tantalum reserves than the medium-sized ones and the red grid