1) 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。
2) strike-slip and thrust
映秀-北川断裂
3) Yingxiu fault
映秀断裂
4) 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。
5) The Qingchuan fault
青川断裂
1.
The Qingchuan fault is an embranchment of the Longmen Mountain fault belt,we have found dextral strike-slip movement of the Qingchuan fault from field survey and rem.
对龙门山北段的青川断裂进行的系统研究发现:断裂具有明显的右行走滑特征,沿断裂发育大量不同规模的水系位错,其中嘉陵江水系位错规模最大,据此可确定青川断裂的最大位移量为17km。
6) Ling-Bei fault
灵北断裂
补充资料：南能北秀
【南能北秀】
（杂语）南宗之慧能，北宗之神秀也。(参见：南宗)
（杂语）南宗之慧能，北宗之神秀也。(参见：南宗)
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