In the areas where one plate is beneath another, stress builds up over time.
被一个板块压在另一个板块之下的区域，压力会随着时间不断累积。
There are some differences of principal stress between secondary tectonic areas.
不同构造区主应力方向存在一定的差异。
Finally, different stress paths and strain areas would lead to different attenuation trends.
但应力路径、应变范围不同其衰减幅度不同。
Finally, different stress paths and strain areas would lead to different attenuation trends.
但应力路径、应变范围不同其衰减幅度不同。
应用推荐