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喀拉通克铜镍矿区位于新疆富蕴县境内,矿区处于库尔提—乌恰深断裂与海子口—卡拉先格尔大断裂交汇点西南约十五公里的地方。由上述两大断裂导出的次一级北西向断裂是含铜镍硫化矿的基性杂岩体的主要控岩构造。沿深断裂侵入的岩浆岩有多次侵入的特点。含矿基性岩体沿北西向呈带状分布。现已发现的岩体有Y_1、Y_2、Y_3、Y_6、Y_7、Y_8、Y_9等,均侵入于下石炭统南明水组一套以正常沉
The Kalatongke copper-nickel mining area is located in Fuyun County, Xinjiang. The mining area is about 15 kilometers southwest of the intersection of the Kurdi-Wuqiand deep fault and the Haizi Kou-Kailashinger fault. The sub-primary north-west fault derived from the above two faults is the main controlled rock structure of the basic complex rock mass containing Cu-Ni sulfide ore. Intrusive magmatic rocks along the deep faults have multiple intrusions. The ore-bearing basic rock mass distributes along the belt in the northwest direction. The rock mass has been found to have Y_1, Y_2, Y_3, Y_6, Y_7, Y_8, Y_9 and so on, all intruding into a set of Lower Carboniferous Nanming water group,