CAJ | 학술논문

新疆塔阿西-塔吐鲁沟铁成矿带处于西昆仑造山带中段的塔什库尔干陆块内，赋矿地层为古元古界布伦阔勒群。成矿带由3个含铁海相火山-沉积盆地和盆间隆起带构成，含铁海相火山-沉积盆地内铁矿产地密布，含铁建造为变质的海相中基性火山岩-流纹岩-凝灰质碎屑岩-碳酸盐岩。中基性火山岩、流纹岩是主要赋矿岩石。塔阿西-塔吐鲁沟铁成矿带的发现为西昆仑造山带内寻找同类铁矿提供了一个范例。
신강탑아서-탑토로구철성광대처우서곤륜조산대중단적탑십고이간륙괴내，부광지층위고원고계포륜활륵군。성광대유3개함철해상화산-침적분지화분간륭기대구성，함철해상화산-침적분지내철광산지밀포，함철건조위변질적해상중기성화산암-류문암-응회질쇄설암-탄산염암。중기성화산암、류문암시주요부광암석。탑아서-탑토로구철성광대적발현위서곤륜조산대내심조동류철광제공료일개범례。
XinJiang Taaxi-Ta Tulugou iron mineralization belt located in the Taxkorgan continental block in the the middle west KunLun orogenic belt, the ore bearing strata are palaeoproterozoic Bulunkuole group. Metallogenic belt is composed of 3 iron containing marine volcano-sedimentary basins and Inter basin uplift zone, in the iron containing marine volcano-sedimentary basin, iron ore producer clouds, iron formation is metamorphic marine Neutral basic volcanic rocks-rhyolite-tuff clastic rock-carbonate rock. Neutral basic volcanic rocks, rhyolite is the main ore bearing rock. Discovery of Taaxi-Ta Tulugou iron mineralization belt provide a paradigm for searching the same iron ore in the West KunLun orogenic belt.