CAJ | 학술논문

新疆塔什库尔干县老并磁铁矿位于塔阿西大断裂西侧，矿体主要赋存于下古生代浅变质的碎屑岩-火山碎屑含铁岩系岩中。矿体多呈层状产出，与地层产状一致，层控作用比较明显。矿石主要为石膏磁铁矿和块状磁铁矿矿石；矿石品位较低(tFe=20%～40%)。该铁矿属沉积变质型铁矿。
신강탑십고이간현로병자철광위우탑아서대단렬서측，광체주요부존우하고생대천변질적쇄설암-화산쇄설함철암계암중。광체다정층상산출，여지층산상일치，층공작용비교명현。광석주요위석고자철광화괴상자철광광석；광석품위교저(tFe=20%～40%)。해철광속침적변질형철광。
laobing Magnetite Mine of tashkurgan, sinkiang is located in the west of taaxi great fault and ore body occurs mainly in the lower Paleozoic shallow metamorphic clastic rocks - volcanic debris iron-bearing rocks. ore bodies are in layered output, consistent with the attitude of stratum, and layer control is obvious. Magnetite ore mainly is gypsum and blocky magnetite ore; ore grade is low (tFe = 20% ~ 40%). the iron ore type belongs to sedimentary metamorphic iron ore.