| 浅析新洲背斜的构造演化与成矿机理 |
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| 引用本文： | 黄谷灿,杨怀顺,姚双秋.浅析新洲背斜的构造演化与成矿机理[J].科技情报开发与经济,2008,18(25):111-113. |
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| 作者姓名： | 黄谷灿 杨怀顺 姚双秋 |
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| 作者单位： | 广两壮族自治区274地质队,广西北海,536005 |
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| 摘 要： | 地应力的作用使新洲背斜发生隆起,在浅表形成相应的劈裂、滑移及挤压区,地应力的不平衡,使辉绿岩岩浆侵入,其析出的含金、锑热液形成锑→金分带性产出,并受地层及构造控制。根据其成因分析,在新洲背斜东部核心区的周边成矿条件较为优越,存在发现新矿床的前景。
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| 关 键 词： | 锑矿床 金矿床 找矿方向 矿床成因 构造演化 新洲背斜 |
The Analysis of Xinzhou Anticline's Structure Evolution and Metallogenic Mechanism |
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| HUANG Gu-can,YANG Huai-shun,YAO Shuang-qiu.The Analysis of Xinzhou Anticline''''s Structure Evolution and Metallogenic Mechanism[J].Sci-Tech Information Development & Economy,2008,18(25):111-113. |
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| Authors: | HUANG Gu-can YANG Huai-shun YAO Shuang-qiu |
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| Institution: | HUANG Gu-can, YANG Huai-shun, YAO Shuang-qiu |
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| Abstract: | The Impact of the crustal stress made the Xinzhou Anticline uplift and form the corresponding crevice, slip band and Squeeze Districts on the earth's surface. The Diabase, which invaded for the imbalance of the stress, is under the controlling of formation and structure, its Hydrothermal separated out the antimony and the gold in turn . According to its causes, the eastern part of the Xinzhou anticline core area surrounding the mineralization has advantageous conditions to discover some new deposits in the future. |
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| Keywords: | Antimony deposit Gold deposit prospecting direction deposit origin structure evolution Xinzhou anticline |
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