| 湘黔地区金刚石找矿之我见 |
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| 引用本文： | 盛学庸.湘黔地区金刚石找矿之我见[J].贵州地质,2011(4):247-253. |
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| 作者姓名： | 盛学庸 |
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| 作者单位： | 贵州地矿局地质科研所 |
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| 摘 要： | 湘黔地区金刚石成矿作用素有＂多期＂、＂多源＂之说。＂多源＂说已为不争事实,系该区开展新一轮金刚石原生矿找矿的依据和前提;笔者质疑＂多期＂说,并指出加里东期为本区的主要金刚石成矿期,是找矿的主攻方向。在具备成矿条件的前提下,成矿后的剥蚀-保存条件将决定矿床的命运和价值。因金刚石原生矿均系幔源火山作用的产物,由此引申出研究...
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| 关 键 词： | 金刚石原生矿 钾镁煌斑岩 加里东期 古剥夷面 指示矿物 重砂法 贵州-湖南 |
My View about Diamond Exploration in Hunan-Guizhou Province |
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| SHENG Xue-yong.My View about Diamond Exploration in Hunan-Guizhou Province[J].Guizhou Geology,2011(4):247-253. |
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| Authors: | SHENG Xue-yong |
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| Institution: | SHENG Xue-yong(Guizhou Institute of Geologic Sciences,Guiyang 550004,Guizhou,China) |
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| Abstract: | Hunan-Guizhou area is one of the diamond metallic deposit area.Multi phase and multi source about the diamond mineralization has been known.Multi source is the accordance and premise for diamond deposit exploration.Multi phase is doubted and Caledonian is the metallogenic period of the diamond deposit in this area,it should be the exploration target.Under the metallogenic condition,the erosion-conservation condition after mineralization decides the density and value of the deposit.Because diamond deposit is the outcome of mantle volcanism,the importance of the condition of erosion-conservation is can be known.In order to increase the efficiency,on the basis of former experiences,everything must be from the actual condition but avoid the foreign model. |
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| Keywords: | diamond deposit lamproite Caledonian ancient denudation surface indicating mineral heavy mineral method |
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