| 南非主要成矿区带的划分及成矿特征 |
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| 引用本文： | 吴兴源,刘晓阳,王杰,任军平,何胜飞,龚鹏辉,刘宇.南非主要成矿区带的划分及成矿特征[J].地质找矿论丛,2015,30(S1):27-45. |
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| 作者姓名： | 吴兴源 刘晓阳 王杰 任军平 何胜飞 龚鹏辉 刘宇 |
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| 作者单位： | 中国地质调查局天津地质调查中心, 天津 300170;中国地质调查局天津地质调查中心, 天津 300170;中国地质调查局天津地质调查中心, 天津 300170;中国地质调查局天津地质调查中心, 天津 300170;中国地质调查局天津地质调查中心, 天津 300170;中国地质调查局天津地质调查中心, 天津 300170;中国地质调查局天津地质调查中心, 天津 300170 |
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| 基金项目： | 中国地质调查局项目"非洲中南部重要矿床地质背景、成矿作用和找矿潜力研究"(编号:1212011220910)及国外风险勘查基金项目(编号:科[2011]D3-04)资助。 |
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| 摘 要： | 南非境内矿产资源种类繁多、储量巨大,其内部的构造单元包括一个太古宙克拉通与一系列元古宙-古生代造山带,以及一个代表弧后前陆沉积系统的卡鲁盆地(狭义)。文章结合区域构造演化与成矿关系,将南非划分为6个Ⅲ级成矿区带:太古宙卡普瓦尔克拉通金-铀、铁-铜-铂族元素、金刚石成矿区,古元古代林波波金-金刚石成矿,古元古代海斯铁-锰成矿带,中元古代那马奎铜-铅-锌多金属成矿,古生代开普褶皱带钨-锡-铜-钼多金属成矿带,古生代-中新生代卡鲁盆地铀-金刚石-砂金成矿区。
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| 关 键 词： | 构造单元 成矿区带 成矿地质特征 南非 |
| 收稿时间： | 2015/9/14 0:00:00 |
| 修稿时间： | 2015/11/3 0:00:00 |
Subdivision of main metallogenic provinces (belts) in South Africa and their metallogenic characteristics |
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| WU Xingyuan,LIU Xiaoyang,WANG Jie,REN Junping,HE Shengfei,GONG Penghui and LIU Yu.Subdivision of main metallogenic provinces (belts) in South Africa and their metallogenic characteristics[J].Contributions to Geology and Mineral Resources Research,2015,30(S1):27-45. |
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| Authors: | WU Xingyuan LIU Xiaoyang WANG Jie REN Junping HE Shengfei GONG Penghui and LIU Yu |
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| Institution: | Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China;Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China;Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China;Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China;Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China;Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China;Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China |
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| Abstract: | There are great variety of mineral resources and huge reserves and geotectonic units, such as a Archean craton, a series of Proterozoic-Palaeozoic orogenic belts and Karoo basin which represents a retro-arc foreland sedimentary system in South Africa. Based on relation of regional tectonic evolution to metallogeny 6 metallogenic belts (areas) III are divided in the country. They are Kaapvaal Archean craton, an Au-U, Fe-Cu-Ni-PGE, diamond area; Paleoproterozoic Limpopo metamorphic belt , an Au-diamond metallogenic belt; Paleoproterozoic Kheis Fe-Mn metallogenic belt; Middle Proterozoic Namaqua Cu-Pb-Zn polymetallic metallogenic belt; Paleozoic Cape Orogenic belt, a W-Sn-Cu-Mo polymetallic metallogenic belt; Paleozoic-Cenozoic Karoo basin, an U-diamond-placer gold area. |
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| Keywords: | tectonic unit metallogenic belt (area) metallogenic characteristics South Africa |
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