1) 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。
2) 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。
3) 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。
4) Qingchuan fault zone
青川断裂带
1.
Qingchuan fault zone is an important tectonic boundary separating the Longmenshan tectonic belt and Motianling tectonic belt.
青川断裂带是一条位于龙门山构造带与摩天岭构造带之间的重要构造边界。
5) Yinchuan buried fault
银川隐伏断层
1.
This paper introduces the result of exploration of the Yinchuan buried fault using the composite drilling section method.
为获取银川隐伏断层近地表断错、上断点埋深、最新活动时代及滑动速率等信息,在浅层地震勘探基础上,沿断层自北向南横跨主断层布施了新渠梢、满春和板桥3条钻孔联合剖面,确定了主断层在3条剖面上的准确位置,获得主断层上断点埋深分别为5·18~8·30m(新渠梢)、5·01~6·50m(满春)和10·0~13·59m(板桥)。
2.
As a late Pleistocene epoch-Holocene active fault,Yinchuan buried fault is one of the active faults which perhaps affect the urban planning and development and earthquake resistance of Yinchuan City seriously.
银川盆地是受断层控制的断陷性盆地,边缘和内部发育了多条断裂带,特别是其内部晚更新世—全新世活动的银川隐伏断层可能对银川市的建设规划和抗震设防影响较大。
6) Qingchuan
青川
1.
The study area situated in the north of longmenshan fault zone belongs administratively to the Qingchuan County of Sichuan province,which is one of the worst-hit mountainous areas in whenchuan earthquake.
研究区(青川县)处于龙门山断裂带北端,是本次地震受灾最为严重的县市之一,由于距南坪、松潘、茂汶、平武等强震区约100公里,兼之断裂带与其相连,故历次地震均受波及,时有损失。
补充资料：青川
1.碧绿的水流。
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