查询词典 earthquake waves

Many towns along Chile's Pacific coast—such as Talcahuano, pictured on March 1, 2010—were devastated by tsunami waves set off by the February 27 earthquake.

智利太平洋沿岸的许多小镇——比如Talcahuano，摄于2010年3月1日——被由2月27日的地震所引发的海啸巨浪所毁坏。

Using maximum coseismic displacement obtained from seismogeological studies and inversions from seismic waves, the recurrence intervals of great earthquakes, such as the 2008 Wenchuan earthquake, can be estimated to be 2000 ~6000 years.

利用地震地质考察和地震波反演得到的最大同震位移可以获得相当于5.12汶川大地震的强震复发周期为2000～6000年。

Using maximum coseismic displacement obtained from seismogeological studies and inversions from seismic waves, the recurrence intervals of great earthquakes, such as the 2008 Wenchuan earthquake, can be estimated to be 2000~6000 years.

利用地震地质考察和地震波反演得到的最大同震位移可以获得相当于5.12汉川大地震的强震复发周期为2000~6000年。

Finally the catastrophe occurs finally, the earthquake initiates the big Tsunami, surmounts 200 meter big ocean waves to break in Bangkok, destroys DORTS, the whole city is snowing.

最後大灾难终于发生，地震引发大海啸，超越 200 米的大海浪冲入曼谷，摧毁捷运，全市落雪。

The most direct cause-effect relationship is that the passage of the seismic waves, generated by the thermonuclear explosion, through the epicentral region in Afghanistan somehow triggered the earthquake.

比较直接的关联有可能是这样的：热核爆炸产生的震波途径阿富汗震中区域时不知为何触发了地震。

The most direct cause-effect relationship is that the passage of the seismic waves, generated by the thermonuclear explosion, through the epicentral region in Afghanistan somehow triggered the earthquake.

最直接的因果关系可能是：热核爆炸产生的震波在经过阿富汗震中区域时以某种方式触发了地震。

Using teleseismic body waves recorded by long period seismograph stations of the global seismic network, the temporal-spatial source process of the June, 4,2000 southern Sumatra M8.0 earthquake, Indonesia, was studied.

利用全球地震台网的长周期地震仪记录到的远震体波反演了2000年6月4日印度尼西亚苏门答腊南部M8.0地震的时空破裂过程。

With this velocity model and broadband records from 5 CDSN stations, we inverted focal mechanisms of Chifeng earthquake on August 16th, 2003 with the "Cut and Paste" method. Then we confirmed focal depth and the source mechanisms by comparing synthetic body waves at teleseismic distance with broadband records of 9 IRIS stations. Our result shows that the best double couple solution of this M w5.2 event is 315°, 64° and 19°for strike, dip and slip angles respectively, the second nodal plane solution is 216°,74°, and 152°. The focal depth is 25±2 km, suggesting that this quake occurred in the lower crust which is much deeper than most continental earthquakes.

我们以此速度结构作为模型，利用中国国家地震台网5个台站的宽频带地震数据，采用CAP方法反演2003年8月16日赤峰地震震源机制解并初步确定震源深度；再利用IRIS 9个台站远震体波数据，通过对比理论计算和观测记录的方法进一步精确确定震源深度并验证反演得到的机制解，得出此次地震矩震级为5.2，震源机制解为：节面I：315°/64°/19°，节面II：216°/74°/152°，震源深度为25±2 km，已深达下地壳。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。