| 中亚古生代造山带成矿作用基本特征 |
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| 引用本文： | 刘德权,唐延龄,周汝洪.中亚古生代造山带成矿作用基本特征[J].西北地质,2001,34(2):1-10. |
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| 作者姓名： | 刘德权 唐延龄 周汝洪 |
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| 作者单位： | 新疆地矿局, |
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| 摘 要： | 中亚成矿域是与环太平洋成矿域、特提斯成矿域媲美的巨型成矿域。其成矿作用带有鲜明的古生代造出带成矿作用特点，在中亚各古生代造山带发展的拉张型过渡壳－洋壳－汇聚型过渡壳－古生代新陆壳的各阶段，形成特定的矿床成矿系列类型，矿床成矿系列类型本身也随着地壳发展，地壳成熟度的提高而有规律地演化。
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| 关 键 词： | 造山带 成矿作用 矿床成矿系列类型 古生代 地壳成熟度 |
| 文章编号： | 1009-6248(2001)02-0001-10 |
The characteristics of mineralization of the Central Asian Paleozoic orogenic zone |
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| LIU De quan,TANG Yan ling,ZHOU Ru hong.The characteristics of mineralization of the Central Asian Paleozoic orogenic zone[J].Northwestern Geology,2001,34(2):1-10. |
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| Authors: | LIU De quan TANG Yan ling ZHOU Ru hong |
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| Abstract: | The Paleozoic metallogenic domain of the Central Asian was a giant metallogenic domain which can compare favourably with the ring Pacific ocean and the Tethys Its mineralization has the manifest singularity of the Paleozoic orogenic mineralization In the every stage that crustal develops tensile transitional, crust oceanic, crust convergent transitional, crust new continental of the Paleozoic orogenic zone in Meddle Asia,it formed various specific metallogenic series type The series type evolved regularly with the raise of the crustal maturity |
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| Keywords: | orogenic zone mineralization metallogenic series type Central Asian Paleozoic |
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