• 责任者：Zang Mei (College of Gology and Mining Engineering Program ; Xinjiang University ; Urumqi 830046 ; China) ; Dong Lianhui
• 刊名：Xinjiang Geology
• 出版年：2013
• 卷期：31(4)
• 关键词：铁矿 ; iron ores ; 角闪岩 ; amphibolites ; 新疆 ; Xinjiang
• 页码：p.275-280
• 图表：6 illus., 1 table, 22 refs.
• 分类号：1001
• issnNo：ISSN1000-8845
• isbnNo：CN65-1092/P

     Baliersi iron deposit is located in Maizi Basin of the south margin of Altay orogenic belt. The orebodies are hosted in the metamorphosed volcaniclastic-sedimentary rocks of the Upper Silurian- Lower Devonian Kangbutiebao For- marion. The orebodies are largely concordant with the bedding of the strata, and the wall rocks are amphibolite, granulite and leptite. Abundant skarn minerals as garnet, diopside, amphibole, epitote, chlorite are widely distributed around the orebodies. LA-ICP-MS U-Pb dating of zircon from the amphibolite in the No.2 orebody wall rock of Baliersi iron deposit has been carried out in this study. The results show that the weighted average ~＇~6PbF~U age of the 32 zircon grains is （385~ 1.6） Ma （MSDW= 1.2）. A combination of the ages of Kangbutiebao Formation in the region limits the Kangbutiebao For- mation is of Late Silurian-Early Devonian, and constraining the age of Baliersi iron deposit to 〈 385 Ma.