| 内蒙古小东沟钼多金属矿床地质特征 |
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| 引用本文： | 吕增尧,赵英福.内蒙古小东沟钼多金属矿床地质特征[J].矿产与地质,2004,18(3):256-259. |
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| 作者姓名： | 吕增尧 赵英福 |
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| 作者单位： | 华北地质勘查局综合普查大队,河北,燕郊,065201 |
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| 摘 要： | 阐述了小东沟钼多金属矿床的矿体、矿化蚀变、硫同位素等地质特征，初步确定成矿物质来源于深源岩浆。矿床属于与燕山早期晚阶段小东沟花岗岩体有关的斑岩型钼矿床—中低温铅锌矿床。
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| 关 键 词： | 钼多金属矿床 地质特征 斑岩型 内蒙古小东沟 |
| 文章编号： | 1001-5663(2004)03-0256-04 |
| 修稿时间： | 2003年5月11日 |
GEOLOGICAL FEATURE OF THE XIAODONGGOU MOLYBDENUM POLYMETALLIC DEPOSIT |
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| LU Zeng-yao,ZHAO Ying-fu.GEOLOGICAL FEATURE OF THE XIAODONGGOU MOLYBDENUM POLYMETALLIC DEPOSIT[J].Mineral Resources and Geology,2004,18(3):256-259. |
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| Authors: | LU Zeng-yao ZHAO Ying-fu |
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| Abstract: | The paper discussed the geologic characteristics of the Xiaodonggou molybdenum polymetallic deposit such as the orebodies, alteration-mineralization and sulfur isotope etc. It is confirmed that the ore was derived from plutonic magma initially. The deposit belongs to the porphyry type molybdenum-mesothermal to epithermal lead and zinc deposit associated with the Xiaodonggou granite in late stage of Early Yanshan period. |
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| Keywords: | molybdenum polymetallic deposit geological feature porphyry type Xiaodonggou Neimenggu |
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