CAJ | 학술논문

卡拉盖雷铜钴金矿区位于新疆西天山伊犁微板块之伊犁裂谷带南缘，那拉提构造带西段。西天山地区位于卡拉库姆-塔里木板块与哈萨克斯坦-准噶尔板块的汇聚地带，自太古宙以来经历了极为复杂的地壳演化史。本文通过地球化学判别图解的投点分析以及与区域地质发展史的对比研究，认为该区大哈拉军山组火山岩的构造背景为大陆弧环境。
잡랍개뢰동고금광구위우신강서천산이리미판괴지이리렬곡대남연，나랍제구조대서단。서천산지구위우잡랍고모-탑리목판괴여합살극사탄-준갈이판괴적회취지대，자태고주이래경력료겁위복잡적지각연화사。본문통과지구화학판별도해적투점분석이급여구역지질발전사적대비연구，인위해구대합랍군산조화산암적구조배경위대륙호배경。
Kalagailei Cu-Co-Au deposit is located along the southern margin of the Ili rift belt in the Ili mi-cro-plate in Western Tianshan Mountain, western part of Nalati tectonic zone, Xinjiang. And Western Tianshan Mountain is situated in the convergence zone of Karakum-Tarim plate and Kazakhstan-Junggar plate. It has a very complex history of crustal evolution since Archean. Through the analysis of geochemical discrimination dia-gram, and the comparison with regional geological development history, the authors suggest that the tectonic set-ting of the igneous rocks in the Dahalajunshan Formation belong to continental arc environment.