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Yuemakeqi Cu deposit, Aletai Co. (Altay Co.), Aletai Prefecture (Altay Prefecture), Yili Hasake Autonomous Prefecture (Ili Kazakh Autonomous Prefecture), Xinjiang Autonomous Region, China
约马克其铜矿, 阿勒泰市 (ئالتاي شەھىرى), 阿勒泰地区 (ئالتاي ۋىلايىتى), 伊犁哈萨克自治州 (ئاپتونوم ئوبلاستىئىلى قازاق), 新疆维吾尔自治区, 中国Copper-polymetallic deposit, hosted in a fault belt in the southern margin of the Altay Mountains and controlled by intrusions of the Yuemakeqi mafic-ultramafic complex distributing along the belt. The latter mainly consist of gabbro, gabbro-diabase, pyroxenite and olivine pyroxenite. The orebodies are hosted in gabbro-diabase; they are stratiform, trend EW and dip south at an angle of 60° to 85°. The deposit is interpreted as having been formed by magmatic differentiation.
Mineral List
| Chalcopyrite 'Chlorite Group' Epidote | Malachite Muscovite var: Sericite 'Olivine' | Pentlandite Pyrite 'Serpentine Group' |
9 entries listed. 5 valid minerals.
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References
Ming Li, Chenxiang Hu, Ziqiang Zhao, Hongqiang Zhang, Zhanyou Ma, and Xiaoran Du (2005): Features of Yuemakeqi copper deposit in Altyn area, Xinjiang Autonomous Region. Geological Survey and Research 28(2), 111-114 (in Chinese with English abstract).
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