断裂的

The former two types are brittle ones, and the fracture strain of pyrolytic carbon matrix is the controlling factor of the strength.

前两种为脆性断裂方式，热解炭基体的断裂应变是这类材料强度的控制因素。

At the end of Oligocene to Miocene, due to lateral extrusion of material in the collisional belt, west Yunnan and adjacent region between the Red River-Ailao Shan and the Saging faults escaped to SSE.

渐新世末—中新世，高原地区的物质侧向挤出，红河—哀牢山断裂和实皆断裂之间的滇西及邻区向南南东脱逸。

A warp skeleton method was proposed to solve the descriptive issue of arbit rary 3D woven composite architecture , with the unit cell being decomposed into subcells/ grids. The subcell vector concept was int roduced to digitalize the 3D architecture , in order to use the 2D database table to store it .

利用经纱脉络描述法解决了任意三维机织复合材料的结构表征问题；提出了单胞分解法与亚胞向量概念，实现了三维结构的二维化、数字化，根据数字表征结果和经典截面假设构造了初始断裂模型；使用一种迭代算法对初始断裂模型进行优化，使纱线束逐步逼近真实形态，进而实现三维实体造型，在此基础上进行网格剖分。

Especially every aspect of mechanical properties of SEN.such as tensile strength,elongation at break,modula and breakenergy etc.,increases synergically whenP/PUC.O.

尤其是聚丙烯酸丁酯/蓖麻油聚氨酯=1/9的SEN，其力学性能的各个方面，如抗张强度，断裂伸长，模量和断裂能等均协同增加。

At last, the stress distribution on whole wafers was analyzed related to the distributaries of oxygen precipitation and dislocations at first time.

同时，还首次指出氮原子对断裂过程可能产生的影响和原因；并首次报导了硅单晶｛112｝＜110＞和｛112｝＜111＞晶向的断裂特征。

The central two sites(the Fenghuang Village site and the Mowan Village site)demonstrate folding scarps which may indicate slipping depth during earthquake.

与此两种断裂陡坎变形不同，中间的两个点则阐述了褶皱陡坎，它们反映了2008年地震中断裂断错在地表以下终止的不同情形。

The post-earthquake geological study shows that the exposed fault planes accompanying with co-seismic scarps usually occurred along the coal seams and carbonaceous shales.

2008年汶川8.0级地震沿龙门山断裂带内的映秀—北川断裂和灌县—安县断裂分别形成约230 km和70 km的地表破裂带。

The micro-morphology of the fracture surface appears to be the inter-granular brittle before sodium corrosion for the rotary swaging and polishing W-specimens.

经高温钠腐蚀后，旋锻钨试样的晶粒长大，断裂应力和显微硬度显著降低；高温钠腐蚀对抛光钨试样的断裂应力和显微硬度似乎无明显影响。

The distribution and formation of epithermal gold deposits in northern Xinjiang are structurally controlled by calderas, craters, diatremes and related faults.

金矿的形成和分布受破火山口、隐爆角砾岩筒、与火山机构有关的断裂以及区域断裂控制。

The main deformational mechanism is cataclasis.

该断裂为地壳浅部构造层次的脆性断裂，主要的变形机制是碎裂作用。

But we don't care about Battlegrounds.

但我们并不在乎沙场中的显露。

Ah! don't mention it, the butcher's shop is a horror.

啊！不用提了。提到肉，真是糟透了。