1) Beichuan fault
北川断层
1.
The Beichuan fault plays an important role in the formation and evolution of Longmenshan thrust zone and Western Sichuan foreland basin, it causes difference between hanging side and heading side of the fault.
龙门山是典型的逆冲断层发育带，北川断层是龙门山逆冲断层系中的主干断层。
2) Qingchuan fault
青川断层
1.
0 Wenchuan earthquake,it becomes an important concern that whether aftershocks direct to Hanzhong along the Qingchuan fault and a strong aftershock also occur.
0级地震后青川断层库仑应力的变化,判明余震的发展趋势,2008年6月2日~28日我们在青川断裂中段阳平关一带开展了断层附近原地应力测量研究,在3个钻孔中分别用水压致裂法和解除法得到了断层上下盘构造应力的大小、方向和分布特征。
3) Chengbei fault
埕北断层
1.
Based on juncture re_processing and interpretation of high_quality 3D seismic data, some new knowledge has been obtained for the southern Chengbei fault in the Chengdao area, that is, a new branch fault is found south of the old fault.
通过对高品质三维地震资料的重新连片处理解释 ,对埕岛油田埕北断层南段部分取得了新的解释结果 ,即在老断层以南又发现一条新的分支断层。
4) the Beichuan-Yingxiu Fault
北川-映秀断裂
1.
A 240km-long co-seismic surface rupture was produced along the Beichuan-Yingxiu Fault during the 2008 Wenchuan earthquake.
0地震在北川-映秀断裂产生了长达240km的同震地表破裂。
5) strike-slip and thrust
映秀-北川断裂
6) the NE trend faults
北东向断层
1.
Appalying the new theory of structural geology, the article focuses on the genesis of the NE trend faulrs and turns out the results that the NE trend faults were formed by expanding gradually because of having been multiply forced.
文中运用构造地质学新理论来研究青岛地区北东向断层的成因。
补充资料：北还登汉阳北原题临川驿
【诗文】：
驱车方向阙，回首一临川。多垒非余耻，无谋终自怜。
乱松知野寺，馀雪记山田。惆怅樵渔事，今还又落然。
【注释】：
【出处】：
全唐诗：卷351-24
驱车方向阙，回首一临川。多垒非余耻，无谋终自怜。
乱松知野寺，馀雪记山田。惆怅樵渔事，今还又落然。
【注释】：
【出处】：
全唐诗：卷351-24
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