1) earthquake inclusion
地震包体
1.
According to the theory of gradient strain, this paper explained the formation of earthquake inclusion,and offered the inclusion width w = 2πl,(lis the charactr length of inside of rock).
采用应变梯度理论，解释了地震包体的形成，给出了包体宽度w＝2πl，其中l是岩石内部特征长度。
2.
By using this model, the class II behavior of rock, the size effect of concrete and the formation of earthquake inclusion are explained.
采用这一模型对岩石Ⅱ类变形曲线、混凝土材料应变软化的尺寸效应和地震包体的形成进行了理论解释。
2) Baotou earthquake
包头地震
1.
T Effects of Differences of Hazard-Bearing Bodies on Earthquake Disasters——A case study on Baotou earthquake and Yao'an earthquake
城乡承灾体差异对地震灾情的影响——以包头地震和姚安地震为例
2.
The seismic damage on power industry buildings in Baotou earthquake on April 3rd in 1996 and its followed strengthening methods are described in this article, meanwhile, seismic damage analysis on power industry buildings is carried out and future design advice is given as well.
本文介绍了1996年5月3日发生的包头地震中电力工业建筑的震害和加固补强方案,并对电力工业建筑进行了震害分析,提出了今后的设计建议。
3.
This paper deals with the behaviors of multistoyr masonry buildingsduring Baotou earthquake.
本文根据现场调查的结果，对包头地震中多层砖房的震害进行了统计，对不同设防情形的多层砖房震害进行了比较;还选取５栋多层砖房进行了抗震验算，并与其实际震害进行了对比分
3) pressure ridge
地震鼓包
1.
A great deal of pressure ridges distribute along the Xidatan strike-slip fault in en-echelon pattern accompanied by varieties of seismic fractures, seismic wedges, seismic scarps and seismic sag-ponds in the Xidatan and Dongdatan valleys in south Kunlun Mts.
在昆仑山南部西大滩与东大滩谷地,沿西大滩活动断裂发育大量串珠状斜列分布的地震鼓包,与不同类型的地震破裂、地震楔、地震陡坎和地震凹陷伴生,在探槽剖面表现为全新世砂土层和晚更新世砾石层的背斜褶皱变形;地震鼓包长轴走向290°~300°,与西大滩活动断裂呈10°~20°交角,锐角指示西大滩断裂左旋走滑运动方向。
4) Western Bao-tou earthquake
包头西地震
5) seismic body wave
地震体波
1.
Wave-type conversion caused by a step topography subjected to inclined seismic body wave;
地震体波斜入射情形下台阶地形引起的波型转换
6) seismic sub-volume
地震子体
补充资料：包析体
peritectoid：合金于冷却时发生包析相变所形成的产物。
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