1) seismic stress
地震应力
1.
Seismic porosity and seismic stress of rocks can be inverted with seismic and geological data based on the theory of two phase medium.
根据双相介质理论 ,使用地震、地质资料反演出地震孔隙率和岩石地震应力。
2.
The paper suggested that the generation of seismic stress is accompanied by the formation of “biaxial strain structure”.
讨论得出地震应力是随着“双向应变结构”的形成而产生的;地震应力主要有压缩应力、拉疏应力及剪切应力的复杂性;地震应力的传递与集中,在本质上就是应变的迁移与应变的转换;地震应力与区域构造应力有生成关系上的联系,也有作用对象与作用目的不同的区别。
2) Earthquake's dynamic stress
地震动应力
3) seismic apparent stress
地震视应力
1.
The average seismic apparent stress and its distribution in Chinese mainland are presented by use of data of medium-strong earthquake from 1900 to 2005.
研究表明:利用地震震级计算的中国大陆地震视应力大小与利用数字地震波资料测定结果相差不大,其空间分布基本一致。
4) seismic stress field
地震应力场
1.
The study results show that the orientation of compressive principal stress is NE and the modern tectonic stress field is in keeping with neotectonic stress field and seismic stress field.
新构造应力场、现代构造应力场、地震应力场趋于一致。
5) seismic stress drop
地震应力降
1.
To obtain the stress level at the earthquake source, this paper sets forth the solution of the stress magnitude at the earthquake source by seismic stress drop and the stress axis deflections before and after large earthquakes.
为求解震源处应力量值,运用大地震造成的应力方向偏转和地震应力降给出了求取震源处应力大小的方法。
6) stress drop
地震应力降
1.
Besides, taking seismic moment (M 0) and stress drop (Δσ)as the scaling parameters, the estimated peak velocity of ground(r·v) is scaled as M 0 1/2 Δσ 1/2 .
假定Q因子随频率线性变化的指数衰减项作为地震波传播距离的非弹性衰减 ,导出用地面运动峰值速度直接估算地震应力降Δσ的关系 :lg (r·v e-qr) =- 6 0 +0 5lgM0 +0 5lgΔσ ,测定了 2 0 0 1年永胜M6 0级地震近场数字地震台网观测的 1 0 0多次余震序列的地震应力降。
补充资料：轧辊残余应力(见轧辊应力)
轧辊残余应力(见轧辊应力)
residual stresses in roll
zhagun eanyu yingli轧辊残余应力(residual stresses in roll)见礼辐应力。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条