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从区域铜镍矿成矿地质背景、矿区地球物理、地球化学特征等方面入手,对图拉尔根①号杂岩体进行岩相、岩石化学特征及矿化蚀变分析,与黄山、香山成型矿床进行对比.证实①号杂岩体岩石组合类型与香山、黄山闪长岩-辉长岩-辉石岩-橄榄岩型岩石组合相当,并具有相似的m/f、Ni/Co及较高的S值含量.矿化主要赋存在角闪橄辉岩相中,主要受杂岩体岩相带及岩相接触带间脆-韧性构造破碎带控制,认为该岩体具有形成岩浆型铜镍矿的成矿远景.
Starting from the geological background of the copper-nickel ore mineralization in the area, the geophysical and geochemical characteristics of the ore district, the petrographic and petrochemical characteristics and mineralization alteration analysis of the Tulargen Complex No. 1 were carried out. Compared with Huangshan and Xiangshan Forming Deposit.It is confirmed that the type of rock assemblage in No.1 complex is similar to that of Xiangshan and Huangshan diorite-gabbro-pyroxenite-peridotite rock with similar m / f, Ni / Co and higher Of S value.The mineralization mainly occurs in the hornblende facies and is mainly controlled by the brittle-ductile structural crust between the lithofacies belt and the contact zone of the lithofacies, which indicates that the rock mass has the characteristics of forming magmatic copper-nickel Mineral prospecting.