原理很简单：一个在之前的强地震中断裂的断层带，一旦再次聚集了足够大的压力后，将可能再次引发同等级别的地震。
The principle is simple: a fault segment that has ruptured in a large quake in the past will-once enough strain has again accumulated-likely fail again in a similar-size earthquake.
简单双原子分子CO与过渡金属间的相互作用，可能导致化学键的断裂与形成，并且引发重要的表面催化反应。
The interaction between simple diatomic molecules such as CO and transition metal surfaces may lead to breaking and making chemical bonds and trigger important surface catalyzed reactions.
目前已提出的韧性断裂准则预测板料成形极限，只在简单轴对称件中得到应用。
At present, some ductile fracture criteria are applied only to predict the forming limit in stamping forming of simple axisymmetric part.
结果表明所给出的单奇异性V形切口的脆性断裂准则有效、简单且便于工程应用。
The findings indicate that the brittle fracture criterion for V-notches with single singularity is valid and simple, so it can be applied to engineering conveniently.
被简化的设计：真空破碎机和接触器是简单在设计比原始的空气断裂设备。
Simplified design: Vacuum breakers and contactors are simpler in design than original air break devices.
根据断裂点公式、距离衰减效应的“简单计算方法”可以定量分析都市区的地域范围。
Using the breaking-point formula and the distance-decay effect, the author develops a quantitative approach called "simple computational method".
晚白垩纪后，构造变形表现为一系列重新活动的基底断裂和新生断裂，褶皱构造简单。
After late Cretaceous, structural deformation shows a series of movable basement fault again and new's fault. The fold structure is very simple.
区域上受多组近东西向断裂控制，区内地层较简单，但岩性复杂，岩浆活动强烈，特别是在雅满苏、沙泉子附近有明显的火山活动中心及残留的火山机构。
The metallogenic district is controlled by a few nearly east and west fractures. In the region, the stratum is simple, but the rock character is complex. The magma activity is fierceness.
在进行大陆板内活动断裂地震危险性定量计算和评估时，不能简单地套用N。
When analyzing and assessing the seismic potential of active faults in an area, we can not simply use the distribution function of earthquakes recurrence intervals given by N.
煤田中部地质构造相对简单，控煤构造样式以褶皱-断裂型为特征，含煤岩系赋存稳定，是有利的勘查开发区段。
Structures in middle zonation are simple and coal-controlled structural style is characterized by fold-thrust pattern, coal measures distributed stable in favor of exploration and development.
盆地内的构造相对简单，断裂以地堑式和阶梯式组合为主，地层仅轻微褶皱且地层厚度及埋深向东及向北减薄、变浅。
Faults styles are mainly graben and step fault. Strata are little folded. Strata thickness and buried depth both decrease eastward and northward.
提出了一种更为简单的估算岩石断裂面粗糙度(jrc)值的分形模型，可用来模拟岩石断裂面剖面线。
A simpler fractal model to estimate the joint roughness coefficient (JRC) is suggested. It can be applied to simulate rock discontinuity profiles.
提出了一种更为简单的估算岩石断裂面粗糙度(jrc)值的分形模型，可用来模拟岩石断裂面剖面线。
A simpler fractal model to estimate the joint roughness coefficient (JRC) is suggested. It can be applied to simulate rock discontinuity profiles.
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