Orebody Characteristics and Deposit Genesis Analysis of the Ore Cluster I of Qunli Iron Mine in Golmud, Qinghai Province, China
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Author(s)
Yuan Kequan, Liu Yongqiang, Ji Shangwen
Corresponding Author
Yuan Kequan
Abstract
Qunli Iron Mine is in the mixed petrified gneiss interbedded with marble and skarn strata of the Lower Rock Formation of the Jinshuikou Group formed in the Lower Proterozoic, and it belongs to a skarn deposit related to migmatization. The regional tectonic structure is located in the central and western sections of the Qimantag-Dulan orogenic belt. The metallogenic belt belongs to the Qimantag-Dulan Hualixi iron, cobalt, bismuth, lead, zinc, copper and silver metallogenic belt. The area has experienced many complicated and strong tectonic movements, and the structural traces of different scales and mechanical properties are well developed. In particular, the northwest-westward compressive and torsional faults constitute the main structural framework in the region, which plays an important role in controlling the distribution of strata, magmatic rocks, metamorphism and mineral resources in various periods.
Keywords
Qunli of golmud city, Iron mine, Ore cluster I, Geological characteristics, Genesis of the deposit
Acknowledgments
None
References
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