XilingoliteChaobuleng Mine, East Ujimqin Banner, Xilin Gol League, Inner Mongolia Autonomous Region, China
Photo: 2008, JGW Latitude: 46°28'47"N
Longitude: 118°40'0"E
朝不楞铁多金属矿床, 东乌珠穆沁旗, 锡林郭勒盟, 内蒙古自治区, 中国
Medium-sized Fe-Zn-Pb-(Ag-Cu-W) skarn, located in the contact zone between a Mesozoic granite and Devonian limestone. The ore bodies are lenticular and lentoid in shape and vary in scale. Alteration is mainly skarnization. Sn, Bi, Ag and Au in ores are recoverable.
References
- Jihong Li (2006): Application of the Integrated Multi-Source Geo-Informations and Marginal Mineralization Theory to Ore Prediction-A Case of Polymetallic Ore Prediction in East Ujimqin County, Inner Mongolia, China. Contributions to Geology and Mineral Resources Research [Dizhi Zhaokuang Luncong] 21, 107-112.
- Fengjun Nie, Wanyi Zhang, Andao Du, Sihong Jiang, and Yan Liu (2007): Re-Os Isotopic Age Dating of Molybdenite Separates from the Chaobuleng Skarn Iron-Polymetallic Deposit,Dong Ujimqin Banner, Inner Mongolia. Acta Geoscientica Sinica 29(4), 315-323.
- Yanjing Chen, Huayong Chen, Khin Zaw, Pirajno, F., and Zengjie Zhang (2007): Geodynamic settings and tectonic model of skarn gold deposits in China: An overview. Ore Geology Reviews 31, 139-169.
- Xiulan Nie and Wanrong Hou (2010): The Discovery of the Diyanqinamu Large-Size Mo-Ag Deposit, Inner Mongolia, and Its Geological Significance. Acta Geoscientica Sinica 31(3), 469-472.
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39 entries listed. 33 valid minerals. 1 type locality (valid mineral).
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