1) deep creep
深部蠕变
1.
Based on the influence of the aging and strain rate of a sloping soil mass on the strength and deformation of the soil mass, as well as the observations of many landslides cases, it has been demonstrated that the mechanism for formation of most landslides can be explained by the deep creep theory.
老化和应变速率对土体强度和变形性质的影响研究,以及野外事例观察,已经证实大多数滑坡的形成机制可以由深部蠕变理论解释。
2) Creep of deep level fault
深部断裂蠕滑
3) Local creep deformation
局部蠕变变形
4) deep deformation
深部变形
1.
On the basis of analysing monitored information of boreholes of seven hydro-engineerings and twenty-seven rock-slopes and landslides obtained by borehole inclinometers,the forms of deep deformation curves may be at least divided into four kinds of curves in category,i.
在分析7个水利水电工程、27个岩石边(滑)坡的钻孔倾斜仪监测资料的基础上,发现深部变形按变形曲线形式至少可分为4大基本类型,即稳定型和3类潜在不稳定型的变形曲线。
5) local creep stress
局部蠕变应力
6) Deep creep-tensile breakage
深部蠕滑-拉裂破坏
补充资料：白银有色金属公司深部铜矿主井和副井
白银有色金属公司深部铜矿主井和副井
白银有色金属公司深部铜矿主井和副井
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