| 新疆温泉县北达巴特斑岩铜钼矿地质特征及成因初探 |
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| 引用本文： | 王玉水.新疆温泉县北达巴特斑岩铜钼矿地质特征及成因初探[J].矿产与地质,2008,22(1):10-14. |
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| 作者姓名： | 王玉水 |
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| 作者单位： | 新疆维吾尔自治区有色地质勘查局703队,新疆,伊宁,835000 |
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| 摘 要： | 北达巴特斑岩铜钼矿产于华力西期流纹斑岩中，矿体呈脉状，铜矿体地表为氧化物，钼矿体主要赋存于深部的流纹斑岩中，其矿化作用呈上铜下钼的双层矿化结构模式，矿化为细脉浸染状。矿床的成因类型为斑岩型铜钼矿。
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| 关 键 词： | 斑岩铜(钼)矿 地质特征 成因 北达巴特 |
| 文章编号： | 1001-5663(2008)01-0010-05 |
| 修稿时间： | 2007年10月15 |
Geological characteristics and genesis discussion of the Beidabate porphyry Cu-Mo deposit in Wenquan County, Xinjiang |
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| WANG Yu-shui.Geological characteristics and genesis discussion of the Beidabate porphyry Cu-Mo deposit in Wenquan County, Xinjiang[J].Mineral Resources and Geology,2008,22(1):10-14. |
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| Authors: | WANG Yu-shui |
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| Institution: | WANG Yu-shui (No. 703 Team of Nonferrous Metals Geo-exploration Bureau in Xinfiang Uigur Autonomous Region, Yining , Xinjiang 835000, China) |
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| Abstract: | The Beidabate porphyry Cu-Mo deposit occurs in Variscan rhyolite porphyry with its orebodies presenting in veins. The surface of Cu orebody is covered with oxide, while the Mo orebody mainly locates in the rhyolite porphyry of deep part. The mineralization presents a double-layer mineralizing structure mode with the upside being Cu mineralization and the underside being Mo mineralization, and occurs in veinlet disseminating state. The genesis type of this deposit is porphyry Cu-Mo deposit. |
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| Keywords: | porphyry Cu （Mo） deposit geological characteristics genesis Beidabate |
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