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艾丁克罗赛岩体位于著名的喀拉通克-南马克苏特铜镍成矿中基性岩带的中部,产于那林卡拉—吉木乃二叠纪叠加型陆相断陷火山盆地,形成于海西晚期后碰撞造山的陆内裂谷构造环境,区域成矿条件十分有利.通过岩石化学和稀土元素地球化学特征研究表明:它属于与铜镍成矿有关的岩体,并经历了较好的深部岩浆分异作用.其铜镍硫化物矿浆熔离作用强度虽比喀拉通克含矿岩体相对偏弱一些,但是仍具有形成比喀拉通克铜镍矿床相对贫化一些的块状硫化物铜镍矿体的成矿条件,而且不排除在其它地区更晚期的隐伏岩体形成较好的铜镍硫化物矿床可能性.
Located in the middle of the well-known basic rock belt in the Kalatongk-Nammaksu copper-nickel mineralization, the Aydın Raussai rock body is produced in the Nalincara-Jimnai Permian superimposed continental facies volcanic basin, Formed in the intracontinental rift tectonic setting of late Hercynian orogeny, and the regional metallogenetic conditions are very favorable.Studies on petrochemistry and REE geochemical characteristics show that it belongs to the rock mass related to copper-nickel mineralization and has experienced more Good deep magmatic differentiation.The copper-nickel sulphide pulp flux is relatively weaker than the Kalatongke ore-bearing rock mass, but it still has a relatively lower degree of depletion than the Kalatongke copper-nickel deposit Massive sulphide Cu-Ni ore bodies do not rule out the possibility of forming better copper-nickel sulphide deposits in more advanced later horizons in other areas.