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Meiling Cu-Au deposit, Hami Co. (Kumul Co.; Qumul Co.), Hami Prefecture (Kumul Prefecture; Qumul Prefecture), Xinjiang Autonomous Region, China

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Name(s) in local language(s): 梅岭铜金矿, 哈密市 (قۇمۇل شەھىرى), 哈密地区 (قۇمۇل ۋىلايىتى), 新疆维吾尔自治区, 中国
Located in the Paleozoic uplift along the southern margin of Tuha basin in eastern Xinjiang, in the superimposed Mesozoic volcanic basin upon the northern part of the Late Paleozoic Dananhu-Tousuquan accretionary arc. The deposit is controlled by NWW-, SN- and EW-trending faults. Host rock is mainly a rhyolitic-dacitic ignimbrite, but Cu-Au mineralization is closely related to quartz porphyry, rhyolitic porphyry and granitic porphyry. Ore-forming styles are dominantly veinlet-disseminations and veinlets, and occasionally stockworks. Hydrothermal alterations are mainly silicfication, sericitization, alunitization, pyrophyllitization, illitization, hydromuscovitization and chloritization.

Mineral List

18 entries listed. 14 valid minerals.

The above list contains all mineral locality references listed on This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.


Yu Miao, Kezhang Qin, Yingxia Xu, Tonghui Fang, Kuishou Ding, and Xingwang Xu (2007): Geological and Fluid Inclusion Characteristics of Meiling Cu-Au Deposit in Kalatage Ore Belt, Eastern Xinjiang, in Comparison with Typical Zijinshan-style HS-epithermal Deposit. Mineral Deposits 26(1), 79-88 (in Chinese with English abstract).

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