| 华南地台盖层褶皱及其形成时期研究 |
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| 引用本文： | 郭福祥.华南地台盖层褶皱及其形成时期研究[J].地质与勘探,1999,35(4):5-7,11. |
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| 作者姓名： | 郭福祥 |
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| 作者单位： | 桂林工学院·桂林·541004 |
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| 基金项目： | 广西壮族自治区自然科学基金资助项目 |
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| 摘 要： | 研究表明：印支运动的褶皱作用非常轻微，认为其导致华南法台盖层全面褶皱的观点是不恰当的。华南地台盖层全面褶皱是由晚三叠世以来多期次继承性造山运动形成的同步一类同步褶皱。主要褶皱时代很晚，在南北太平洋大地构造域是晚侏罗世至中始新世，在特提期大地构造域是中晚始新世之交。
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| 关 键 词： | 华南地台盖层 印支运动 继承性造山运动 中新生代 |
FOLDING OF COVER OF SOUTH CHINA PLATFORM AND ITS FOLDING AGE |
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| Guo Fuxiang.FOLDING OF COVER OF SOUTH CHINA PLATFORM AND ITS FOLDING AGE[J].Geology and Prospecting,1999,35(4):5-7,11. |
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| Authors: | Guo Fuxiang |
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| Abstract: | The recent studies show that the overall folding of the cover of South China platform can not caused by the Indosinian week folding in south China but caused by multiphase inherited orognies after late Triassic. The principal folding is quite late. In the northwest Pacific domain, the folding age is from Late Jurassic to Middle Eocene, and in the Tethys domain it is between Middle and Late Eocene. |
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| Keywords: | cover of south China platform indosinian tectogenesis inherited orogeny Meso-Cenozoic |
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