regional stress meaning in Chinese
区域应力
Examples
- The formation and evolution of liaohe meso - cenozoic basin were controlled by the variation of different regional stress field
摘要中新生代辽河盆地的形成和发展受控于多期区域应力场变化。 - The inversion confirms that plate boundary actions are main factors controlling the regional stress field , and spreading forces of mountains and seashores are another important factor
同时显示了板块在垂直载荷下的弯曲对局部水平应力场造成相当的影响。 - According to guibin - zhang et . recent research hi this aspect , we propose a model in which the mountain root and lithoshpheric root may contribute more to the regional stress system in collision mountain ranges
Bott 、高锐和张贵宾等一批学者已经从理论或数值模拟方面对岩石圈根进行了研究，在这些研究的基础上，本文明确提出岩石圈根拖曳模式。 - The variation of regional stress field can be genetically interpreted by the rotation speed variation of the earth and its impact on the movement of lithosphere plate and deep processes of the earth , it is also related to the earlier structural feature and boundary of the basin
区域应力场变化可以用地球自转速度变化引起的岩石圈板块活动及触发的深部过程来解释，亦与先期构造形迹和盆地边界条件有关。 - The surface loading of the mountains and the associated root of thickened crust produce horizontal deviatoric tension in the strong upper crust . in contrast , the deep , dense lithospheric root and its associated downflexing of the surface produce horizontal compressive deviatoric stress in the strong near - surface layer . the actual state of stress in the strong layer of the upper crust is the combined effect of these two opposite stress systems together with bending and other local and regional stresses such as due to ridge push
模拟结果表明：由于均衡机制，造山带下部的低密度山根促使地壳隆升、造山，山根是地壳刚性层中张性构造应力的主要力源；与此相反，冷的高密度岩石圈向软流圈插入、拆离、下沉，从而形成岩石圈根，它引起挤压造山和岩石圈地幔物质的重新调整，也是地壳刚性层中挤压性构造应力的主要力源。