1) faulted depression
裂陷运动
2) taphrogenesis
[,tæfrəu'dʒenisis]
张陷断裂运动
3) chasmic activities
裂陷活动
1.
Shelincuo and Bangecuo extensional lake basins in the northern pa rt of Tibet and present chasmic activities;
藏北地区色林错、班戈错湖盆扩张及现代裂陷活动
4) moving crack
运动裂纹
1.
In this paper the stress intensity factor of a semi infinite moving crack under the concentrated force is derived.
导出了集中力作用下半无限长运动裂纹的应力强度因子,建立了描述裂纹扩展速度较小时材料动态裂纹特性的数学模型,研究了材料动态断裂性能对裂纹运动的影响,得到了一些有意义的结
2.
By applying the theory of complex function and the principle of strain energy,the present paper obtains an asymptotic expansions for the fields of thetip of a Ⅲ-mode curved moving crack.
本文用复交函数理论及应变能原理,导出了Ⅲ型曲线运动裂纹尖端场的渐近展开式。
3.
In this paper the anti-plane moving crack in non-homogeneous elastic materials is studied by an analytical method.
用解析方法研究了非均匀弹性材料中反平面运动裂纹问题。
5) fault movement
断裂运动
1.
Changling fault depression is continental basin of volcanic-sedimentary rock,fault movement is key factor controling volcanic activity and plane distribution of volcanic rock.
石油地球物理勘探 ,2 0 0 2 ,37(3) :2 91~ 2 94 长岭断陷为陆相火山—沉积岩盆地 ,断裂运动是控制火山活动及火山岩平面分布的主要因素。
6) rhaegmageny
扭裂运动
补充资料:陷裂
1.陷落坼裂。
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