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首页> 外文期刊>Australian Journal of Earth Sciences >Metallogeny of Siberia: tectonic, geologic and metallogenic settings of selected significant deposits*
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Metallogeny of Siberia: tectonic, geologic and metallogenic settings of selected significant deposits*

机译：西伯利亚的成矿作用：某些重要矿床的构造，地质和成矿环境*

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Siberia has a prominent position in Russia, in terms of mineral resources and mineral production including copper, nickel, PGM's, uranium, molybdenum, tungsten, tin, manganese, gold, silver, lead, tantalum-niobium, rare earths, diamonds and many other mineral commodities. These resources are represented by a vast array of mineral systems and deposit styles in their respective terranes spanning the Precambrian and Phanerozoic geological history. These mineral systems include VHMS and SEDEX lead-zinc, orogenic gold, sediment- and shear-zone hosted to intrusive-related silver to silver-tin, alkaline gold to gold-uranium and uranium, porphyry copper and copper-molybdenum, epithermal gold, gold-silver, silver, gold-antimony, mercury, uranium-fluorite, various granite-related deposits (W, Mo, Sn, Be, Ta, Co-Ni, etc.) including those associated with peralkaline granites (Nb-Ta-Zr-REE), skarn iron, lead-zinc, gold, tungsten, carbonatite tantalum-niobium, niobium-REE and REE, magmatic copper-nickel-PGM sulfide, PGM and mafic intrusion-hosted iron-titanium-vanadium deposits, and diamondiferous kimberlites. Some deposits are large and superlarge including the well-known Noril'sk nickel-copper-PGM and Udokan copper deposits, the Sukhoi Log, Olympiada, Nezhdaninskoe, Kubaka, Kupol gold deposits, the Dukat and Prognoz silver deposits, and the Yakutian diamondiferous kimberlites. Apart from the above-mentioned giant deposits, several others are poorly known and/or unknown to western geoscience. The study of these mineral systems can significantly contribute to our further understanding of the metallogeny of cratons and orogenic belts, orogenic collages, and anorogenic settings. This provides additions to, and further development of, existing classifications and genetic models of mineral systems, allowing researchers to elucidate unknown or poorly studied mineral systems and styles found in Siberia, and to search for some other important styles that appear to be missing, although they are present in other regions with similar geological and tectonic settings. View full textDownload full textKEY WORDSmetallogeny, mineral deposits, Siberia, tectonic settingsRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/08120099.2010.505277
机译：在矿产资源和矿产方面，西伯利亚在俄罗斯具有领先地位，包括铜，镍，铂族金属，铀，钼，钨，锡，锰，金，银，铅，钽-铌，稀土，钻石等矿物商品。这些资源由横跨前寒武纪和生代时代的地质历史的各种地层中的大量矿物系统和矿床样式表示。这些矿物系统包括VHMS和SEDEX铅锌，造山金，沉积带和剪切带，这些带侵入性相关的银与银锡，碱性金与金铀和铀，斑岩铜和铜钼，超热金，金-银，银，金-锑，汞，萤石铀，各种与花岗岩有关的矿床（W，Mo，Sn，Be，Ta，Co-Ni等），包括与高碱性花岗岩（Nb-Ta- Zr-REE），矽卡岩铁，铅锌，金，钨，碳酸盐钽-铌，铌-REE和REE，岩浆铜-镍-PGM硫化物，PGM和镁铁质侵入岩型铁-钛-钒矿床和含钻石的金伯利岩。一些矿床是大型和超大型矿床，包括著名的Noril'sk镍铜-PGM和Udokan铜矿床，Sukhoi Log，Olympiada，Nezhdaninskoe，Kubaka，Kupol金矿床，Dukat和Prognoz银矿床以及Yakutian含钻石的金伯利岩矿床。 。除上述巨型矿床外，西方地球科学对其他几个矿床也知之甚少。这些矿物系统的研究可以极大地帮助我们进一步了解克拉通和造山带的成矿作用，造山拼贴和造山环境。这为现有的矿物系统分类和遗传模型提供了补充和进一步的发展，使研究人员可以阐明在西伯利亚发现的未知或研究不足的矿物系统和样式，并寻找其他一些似乎遗失的重要样式。它们存在于其他地质和构造背景相似的地区。查看全文下载全文关键词金属学，矿床，西伯利亚，构造设置相关变量var addthis_config = {ui_cobrand：“泰勒和弗朗西斯在线”，servicescompact：“ citeulike，netvibes，twitter，technorati，delicious，linkedin，facebook，stumbleupon，digg，google，更多”，发布号：“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/08120099.2010.505277

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