| 辛河斌.内蒙古白乃庙铜多金属矿床地质特征及成因讨论[J].地质找矿论丛,2006,(4):236-240,298 |
| 内蒙古白乃庙铜多金属矿床地质特征及成因讨论 |
| GEOLOGICAL CHARACTERISTICS AND GENESIS OF BOIN SUM COPPER PLYMETAL DEPOSIT IN INNER MONGOLIA |
| 投稿时间：2005-11-08 |
| DOI：10.6053/j.issn.1001-1412.2006.4. 003 |
| 中文关键词: 白乃庙铜多金属矿床 地质特征 成因讨论 内蒙古自治区 |
| 英文关键词:Boin Sum Cu polymetal diposit geological characteristics genetic discussion Inner Mongolia |
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| 中文摘要: |
| 白乃庙铜多金属矿床产于遭受了韧性变形的白乃庙群变质火山岩和花岗闪长斑岩中,矿床的地质-地球化学特征表明,除了赋矿围岩不同外,南、北两矿带中的其他地质特征基本一致,成矿流体具有深源特点,韧性剪切对成矿有叠加改造作用,连续发生的斑岩成矿作用和韧性剪切成矿作用产生于加里东期。矿床为复因多位的铜(钼)多金属矿床。 |
| 英文摘要: |
| Boin Sum copper polymetal deposit occurs in meta-volcanic rock of Boin Sum group and granodioritic porphyry that were exposed to ductile deformation.Geological and geochemical characteristics of the deposit show that the south,morth ore zones are basically the same in geological characteristics except for their host rocks.Ore fluid all comes from depth and mineralization are all overprinted by ductile shearing.The ductile shearing and porphyry ore-forming processes took place continuously in Caledonian period.The deposit is a complex multi-genesis and multi-emplacement Cu(Mo) polymental deposit. |
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