| 台湾海峡西岸及台湾岛的现代升降运动 |
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| 引用本文： | 毕福志,袁又申,温庆兰.台湾海峡西岸及台湾岛的现代升降运动[J].地球科学与环境学报,1987(2). |
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| 作者姓名： | 毕福志 袁又申 温庆兰 |
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| 作者单位： | 国家地震局地壳应力研究所
(毕福志，袁又申)，国家海洋局海洋情报研究所(温庆兰) |
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| 摘 要： | 台湾海峡西岸及台湾岛的现代升降运动,目前正处于以上升为主兼有局部下降的活动阶段。并以升降幅度大、升降速率快、断块或褶皱断裂构造升降差异显著为其基本特征。其百年内升降幅度最大值可达6～7m,升降速率一般为2～3cm/y(最大值可达10cm/y),堪称世界之冠。
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| 关 键 词： | 台湾海峡西岸 台湾岛 现代地壳升降运动 升降幅度 升降速率 |
THE UPLIFT- DESCENT MOTION ON THE WEST COAST OF THE TAIWAN STRAIT AND ON THE TAIWAN ISLAND |
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| Bi Fuzhi Yuang Youshen.THE UPLIFT- DESCENT MOTION ON THE WEST COAST OF THE TAIWAN STRAIT AND ON THE TAIWAN ISLAND[J].Journal of Earth Sciences and Environment,1987(2). |
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| Authors: | Bi Fuzhi Yuang Youshen |
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| Abstract: | The crustal motion on the west coast of the Taiwan Strait and on he Taiwan lsland is at present characterised by a predominance of uplift. Des-tccnt is only locally observed the uplift-descent scale ranging 6 to 7m within a hundred years is large,the uplift-descent rate up to 10cm/y(in general 2-3cm/y ) is rapid.These may be the largest all over the world. |
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| Keywords: | uplift-descent motion west coast of Taiwan Strait Taiwan lsland |
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