| 根据沉积相研究讨论高院断层的时代 |
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| 引用本文： | 周洪庆,毛家仁.根据沉积相研究讨论高院断层的时代[J].贵州工业大学学报(自然科学版),1997,26(2):17-22. |
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| 作者姓名： | 周洪庆 毛家仁 |
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| 作者单位： | 贵州工业大学资源工程系 |
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| 摘 要： | 根据贵阳乌当地区高院断层两侧早奥陶世地层的沉积相分析，首次提出了高院断层的最初形成时代为早奥陶世时期在后期的构造运动中该古断裂发生了两次显示的复活。
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| 关 键 词： | 沉积相 古断裂 早奥陶世 断裂复活 构造运动 |
A DISCUSSION ON THE GROWTH PERIOD OF GAOYUAN FAULT THROUGH RESEARCH OF SEDIMENTARY FACIES |
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| Zhou Hongqing,Mao Jiaren.A DISCUSSION ON THE GROWTH PERIOD OF GAOYUAN FAULT THROUGH RESEARCH OF SEDIMENTARY FACIES[J].Journal of Guizhou University of Technology(Natural Science Edition),1997,26(2):17-22. |
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| Authors: | Zhou Hongqing Mao Jiaren |
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| Abstract: | According to the analysis of sedimentary facies of Early Ordovician in Wudang,Guiyang,the authors suggest that the initial growth of Gaoyang fault took place in Early Ordovician and that the palae-fault experienced two revivals in the later tectonic movement. |
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| Keywords: | sedimentary facies palae-fault Early Ordovician fault reviving |
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