1) Southern Longshou fault
龙首山南缘断裂
2) Southern marginal fault zone of Taihangshan Mountains
太行山南缘断裂带
3) southern marginal fault belt of the Narat Mountain
纳拉提山南缘断裂带
4) South Altyn border faults zone
南缘断裂带
5) Longmenshan fault
龙门山断裂
1.
In this paper by utilizing the mobile short-line leveling data across the Longmenshan fault the variation characteristics at each observation site before and after the Wenchuan earthquake are analyzed.
利用跨龙门山断裂的流动短水准观测资料分析了汶川地震前后各测点的变化特征。
2.
The fitting results shows that:the wholly velocities of Xianshuihe and Longmenshan fault is 8.
研究表明鲜水河断裂、龙门山断裂的整体运动速率分别为8。
3.
The results show that before the earthquake the regional deformation were staged,in detail,its differential elevation and subsidence weakened and the movement of Longmenshan fault turned from active to locked,after the earthquake,the earthquake effect spreaded north-east ward along the Longmenshan fault mainly and the co-seismic deformation nearby the after s.
结果表明:震前,区域垂直形变表现出某种阶段性,升降差异运动由剧烈向减弱变化,龙门山断裂活动也由活跃向闭锁转换;震后,地震影响主要沿龙门山断裂带向北东方向扩展,余震区附近同震形变显著。
6) Longmen Shan faults
龙门山断裂
1.
As a preliminary result,we measured the fast polarization azimuth and time delay of the Ps converted wave in the receiver functions at 4 stations on both sides of Longmen Shan Faults.
作为初步结果,得到了龙门山断裂两侧4个宽频带流动台站的接收函数莫霍面Ps转换震相快波方向和分裂时间延迟。
补充资料：龙首山
见走廊北山。
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