| 单词 | 断层 |
| 释义 | 〔hade〕The angle of inclination from the vertical of a vein, fault, or lode.倾斜余角：因矿脉，断层或矿井倾斜而与垂直面形成的角度〔mylonite〕A fine-grained laminated rock formed by the shifting of rock layers along faults.糜棱岩：由岩石层沿断层转移而形成纹理细密的叠层岩〔microgravity〕A minute shift in gravity that can occur through geologic factors in a region, such as the movement of the earth's crust along fault lines.微重力移动：经由一个地区的地质因素所发生重力的微小转移，例如沿着断层所发生的地球板块移动〔displacement〕The distance between the two sides of a fault. Also called dislocation 断层两侧的距离 也作 dislocation〔slip〕The relative displacement of formerly adjacent points on opposite sides of a fault.位移：以前相邻的两个点在一个断层的两侧的相对错位〔massif〕A large section or block of the earth's crust that is more rigid than the surrounding rock and has been moved or displaced as a unit.断层地块：一大块比周围岩石更坚硬的、曾发生过整块位移的地壳〔pit〕To mark with cavities, depressions, or scars:使凹下：使有洞、凹地或断层：〔thread〕"More than 90 geologic faults thread the Los Angeles area"(Science News)“洛杉矶地区遍布着90多个地质断层”(科学新闻)〔slickenside〕A polished, striated rock surface caused by one rock mass sliding over another in a fault plane.擦痕面：在断层面上由于一块岩石从另一块岩石上面滑过造成的磨光的、有细槽的岩石面〔neotectonics〕A technique for predicting earthquakes that involves measuring the rate of slippage of landmarks along faults.新地体构造学：以测量断层地标滑动率来预测地震的技术〔displacement〕The relative movement between the two sides of a fault.断层位移：断层两侧的相对位移〔earthquake〕A sudden movement of the earth's crust caused by the release of stress accumulated along geologic faults or by volcanic activity. Also called seism ,temblor 地震：由于地质断层积聚的压力被释放或由于火山活动引起的地壳的突然变动 也作 seism,temblor〔escarpment〕A steep slope or long cliff that results from erosion or faulting and separates two relatively level areas of differing elevations.峭壁，崖：由于腐蚀或断层作用，在两个相对海拔不同的水平地区产生的急斜面或高大的悬崖〔diastrophism〕The process of deformation by which the major features of the earth's crust, including continents, mountains, ocean beds, folds, and faults, are formed.地壳变动：地壳上大陆、山脉、海床、褶皱和断层等主要地貌形成的变形过程 |
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