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青藏高原隆升的潮汐—均衡模式
A Tide--Isostasy Model for the Uplift of Qinghai--Tibet Plateau
【摘要】 潮汐和厄尔尼诺事件使东西太平洋海面高度分别升降 6 0cm ,水均衡作用使洋壳反向升降2 0cm。由此形成东西太平洋地壳跷跷板运动。这是地震火山群发事件与厄尔尼诺事件一一对应的原因。发生在印度洋的同样过程是青藏高原隆升的原因。剥蚀沉积也会产生陆海地壳的跷跷板运动。计算表明 ,5 0年的剥蚀沉积作用施加在陆海地壳两端的力矩为M =4 .36× 10 14 N·m ;相当于在陆海地壳两端施加的反向力 p =4 .36× 10 8N。这两种跷跷板运动相互加强 ,是青藏高原隆升的基本动力。
【Abstract】 Tides and El Nino events make the oceanic water in East Pacific Ocean and West Pacific Ocean going up and down 60 cm oppositely, which makes oceanic crust fall or rise 20 cm. It is the reason why El Nino events are interrelated with the earthquakes and volcanoes. This phenomenon is just like "seesaw". The process occurs not only in Pacific Ocean, but also in Indian Ocean. This may be one of the reasons for the uplift of Qinghai--Tibet Plateau. The denudation and sediment also make the crust move like seesaw. According to the calculation, the moment (M) brought to bear on the two sides of continental and oceanic crust in fifty years is about 4.36× 10 14 N·m.
【Key words】 Qinghai--Tibet Plateau; tides; isostasy; El Nino; earthquake swarms;
- 【文献出处】 世界地质 ,World Geology , 编辑部邮箱 ,2003年02期
- 【分类号】P312.3
- 【被引频次】8
- 【下载频次】93