1) width of surface rupture
地表破裂带宽度
2) Surface fault width of earthquake
地表破裂宽度
3) surface rupture zone
地表破裂带
1.
From north to south,most of the widths of intense surface rupture zones are less than 40m,and above 1/2 are between 10～30m.
0级地震地表破裂带的实地调查,龙门山断裂带的中央断裂与前山断裂地表破裂带宽度自北向南一般<40m。
2.
Based on the latest displacement of Huoshan piedmont fault,Mianshan west-side fault and Taigu fault obtained from the beginning of 1990′s up to the present,the characteristics of distribution and displacement of surface rupture zone of the 1303 Hongtong M =8 earthquake,Shanxi Province are synthesized and discussed in the paper.
综合 2 0世纪 90年代初在霍山山前断裂和近年在绵山西侧断裂和太谷断裂获取的最新调查资料 ,讨论了 130 3年山西洪洞 8级地震地表破裂带的展布和位移特征 。
3.
To know the shallow geological structures under the surface rupture zone,a high-resolut.
此项探测研究以出现在什邡市师古镇附近的疑似地震地表破裂带为切入点,通过采用可控震源以及高精度的浅层地震反射勘探方法,获得了深度15～800m范围内高分辨率的地下结构和构造图像。
4) surface rupture
地表破裂带
1.
Its surface rupture occurs on the Beichuan-Yingxiu and the Jiangyou-Guanxian faults,with the lengths of 200km and 70km,respectively.
地表破裂带的最大挤压缩短量为3。
2.
Besides the huge casualties and property losses, a most complicated yet longest thrust-type co-seismic surface rupture zone was developed in the quake-hit area.
0),地震不仅造成巨大的人员伤亡和财产损失,并形成了迄今为止空间上分布最为复杂、长度最大的逆冲型同震地表破裂带。
5) seismic surface deformation
地震地表破裂带
1.
Primary study on seismic surface deformation and faulting behavior of Central Fault (Beichuan-Yingxiu Fault) is done by methods such as topographic analysis, field geological investigation, trench excavation, geological profile analysis and so on.
目前对其活动速率、活动性、强震复发周期以及震后其地震地表破裂带特征等重要的科学问题上都还没有统一的认识。
6) Shunyi ground rupture zone
顺义地表破裂带
补充资料：地表
1.地面，大地的表面。 2.指陆地的边际。 3.指地球的表面，即地壳的最外层。
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