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地质科学  1999, Vol. Issue (4): 397-404    DOI:
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初议中亚成矿域
涂光炽
中国科学院地球化学研究所, 贵阳550002
ON THE CERTRAL ASIA METALLOGENIC PROVINCE
Tu Guangzhi
Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002
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摘要 给出了中亚成矿域的地质含义与地理范围。此巨型成矿域以发育中、晚元古代及晚古生代成矿作用为其特点。以超大型矿床为重点,并主要围绕金、铜讨论了中亚成矿域6种类型矿床的时空展布。近年取得的进展说明,中亚成矿域在矿产资源优势与潜力方面并不亚于环太平洋成矿域及特提斯成矿域。
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涂光炽
关键词中亚成矿域   黑色岩系矿床   块状硫化物矿床   斑岩矿床   陆相火山岩金矿床   与富碱侵入岩有关矿床   砂岩铜矿床     
Abstract: The Central Asia Metallogenic Province is referred to areas situating between the Siberian craton to the north and the Sino-Korean, the Tarim and other cratons to the south. This metallogenic province is characterized by the Mid-Late Proterozoic and the Late Paleaozoic mineralizations. The spatial and temporal regularities of six important types ore deposits with special reference to Cu and Au super-large ones are discussed. It follows from the discussion that the Au-PGE-Ag-W deposits in carbonaceous formations and the massive sulfide deposits are highly perspective, while the porphyry deposits, the rulaesial volcanics-hosted Au deposits, the ore formations related to alkaline-rich intrusive rocks and the sandstone Cu deposits are also important for this particular province. With respect to ore potentiality, the central Asia Metallogenic Province occupies a position not less significant than the circum-Pacific and the Tethys Metallogenic Provinces.
Key wordsCentral Asia Metallogenic Province   Ore deposits in Carbonaceous formations   Massive sulfide deposits   Porphyry deposits   Volcanics-hosted Au deposits   Ore deposits related to alkaline-rich intrusive rocks   Sandstone Cu deposits   
收稿日期: 1999-02-20;
引用本文:   
涂光炽. 1999, 初议中亚成矿域. 地质科学, (4): 397-404.
Tu Guangzhi. ON THE CERTRAL ASIA METALLOGENIC PROVINCE[J]. Chinese Journal of Geology, 1999, (4): 397-404.
 
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[1] 李红阳, 李英杰, 侯增谦, 杨竹森, 蒙义峰, 曾普胜, 徐文艺. 安徽新桥块状硫化物矿床地球化学特征[J]. 地质科学, 2005, (3): 337-345.
[2] 钟宏, 胡瑞忠, 叶造军. 云南大平掌铜-多金属矿床成矿金属来源初探[J]. 地质科学, 2001, (1): 72-82.
 
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