| 武当地区南北向构造及控矿 |
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| 引用本文： | 刘兴义.武当地区南北向构造及控矿[J].资源环境与工程,1997(1). |
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| 作者姓名： | 刘兴义 |
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| 作者单位： | 鄂西北地质矿产调查所 |
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| 摘 要： | 武当地区存在一种由褶皱断裂组成的南北向构造。形成时期为加里东─华力西旋回，并与武当西部镇旬古生代沉积盆地有着成生联系，扬子板块北缘的南北向裂陷或隆起，属东西向构造相互转换的产物。南北向构造是武当地区矿床的重要控矿构造。
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| 关 键 词： | 武当地区 南北向构造 控矿构造 |
THE N-S-TRENDING TECTONICS IN WUDANG AREA AND ITS CONTROL OVER ORES |
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| Liu Xingyi.THE N-S-TRENDING TECTONICS IN WUDANG AREA AND ITS CONTROL OVER ORES[J].Resources Environment & Engineering,1997(1). |
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| Authors: | Liu Xingyi |
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| Abstract: | In Wudang area the N-S-trending tectonics, composed of faults and folds, formed during Caledonian-Hercynian cycle and are genetically related with the Zhenxun sedimentary basin of Western Wudang. The N - S - trending depression or uplift in north boundary of the Yangtze Plate, resulted from the transmission of the E - W - trending tectonics, are very important ore - controlling tectonics in the area. |
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| Keywords: | Wudang area N-S-trending tectonics Ore - controlling tectonics |
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