| 贵州紫云运动与泥盆纪末华南板块海退事件的因果关系研究 |
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| 引用本文： | 牛新生,徐立明.贵州紫云运动与泥盆纪末华南板块海退事件的因果关系研究[J].华南地质与矿产,2007(1):46-50. |
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| 作者姓名： | 牛新生 徐立明 |
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| 作者单位： | 中国地质大学研究生院,武汉,430074 |
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| 摘 要： | 紫云运动是贵州境内发生于泥盆纪末石炭纪初的一次以地壳相对垂直抬升为主要特点的构造运动。经对比研究,发现紫云运动受控于全球海平面下降和区域构造沉降的联合作用,其断裂特点与区域断裂构造特点相一致,且紫云运动与广西、湖南境内的柳江运动具有时间上的一致性。
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| 关 键 词： | 紫云运动 海退事件 因果关系 |
| 文章编号： | 1007-3701（2007）01-0046-05 |
| 收稿时间： | 2006-08-30 |
| 修稿时间： | 2006年8月30日 |
Research on Causality of Guizhou Ziyun Movement and the Regression of Late Devonian South China Plate |
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| NIU Xins-heng, XU Li-ming.Research on Causality of Guizhou Ziyun Movement and the Regression of Late Devonian South China Plate[J].Geology and Mineral Resources of South China,2007(1):46-50. |
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| Authors: | NIU Xins-heng XU Li-ming |
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| Abstract: | Guizhou Ziyun movement occurred from last stage of late Devonian to initial stage of early Carboniferous,which is characteristic by the relatively vertical raising of lithosphere.After comparing and studying,we found that Ziyun movement is controlled by the combination of global sea level regression and region tectonic sinking.It represents with consistence of local fracture and region fracture.In addition,Ziyun movement and Liujiang movement happened in Guangxi and Hunan,which occurred in the same time. |
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| Keywords: | Ziyun movement regression causality |
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