【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。更多还原

【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.更多还原