✔ 最佳答案
At least 68,800 people killed and severe damage in the Dujiangyan-Mianzhu-Mianyang area. Landslides blocked roads and buried buildings in the Beichuan-Wenchuan area.
The Sichuan earthquake of May 12, 2008, occurred as the result of motion on a northeast striking reverse fault (逆斷地層) or thrust fault on the northwestern margin of the Sichuan Basin. The earthquake's epicenter and focal-mechanism are consistent with it having occurred as the result of movement on the Longmenshan fault (龍門山斷層) or a tectonically related fault. The earthquake reflects tectonic stresses resulting from the convergence of crustal material slowly moving from the high Tibetan Plateau (青藏高原), to the west, against strong crust underlying the Sichuan Basin and southeastern China.
On a continental scale (大範圍來說), the seismicity of central and eastern Asia is a result of northward convergence (聚合) of the India plate (印度板塊) against the Eurasia plate (歐亞板塊)with a velocity of about 50 mm/y. The convergence of the two plates is broadly accommodated by the uplift of the Asian highlands and by the motion of crustal material to the east away from the uplifted Tibetan Plateau.
The northwestern margin of the Sichuan Basin has previously experienced destructive earthquakes. The magnitude 7.5 earthquake of August 25, 1933, killed more than 9,300 people.