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crust fracture相关的网络例句

查询词典 crust fracture

与 crust fracture 相关的网络例句 [注:此内容来源于网络,仅供参考]

A geologic block fault is a fracture in the Earth's crust causing blocks of land to move up or down.

地质块断裂故障是在地壳造成块土地将上涨或下跌。

Based on this, the relation between fracture fractal dimension and the Earth crust activity was discussed.

在此基础上,讨论了断裂尺度分形维数与地壳活动性的关系。

Analyzing the relation between earthquake and structure distortion, main fault belt, crust, upper mantle, ground fracture, hotspring, geotherm, conductance frame, stress state in Guanzhong area is analyzed with earthquake mechanism, isoseismal line, crustal stress measure, fault displacement measure, and simulating test results. Earthquake formation mechanism is discussed with dynamics mechanism in Guanzhong base. There are 3 forces and a good medium environment, which are main reasons caused earthquake happened in Guanzhong area. The first force is NE and NEE level extrusion one which is parallel with long axis of Guanzhong base. The second one is level strain which is vertical with long axis of the base.

对地震与构造形变、主要断裂带、地壳及上地幔、地裂缝、温泉和地热、电性结构等关系进行了分析研究,通过震源机制解、地震等烈度线、地应力测量、断层位移测量及模拟试验等成果,分析了关中地区的地应力状态,从关中盆地的动力学机制,对该区的地震成因机制进行了探讨,认为与关中盆地长轴平行的NE和NEE向的水平挤压力、与盆地长轴方向垂直的水平张力及地幔上涌力三组力的作用,加之壳内高导层这一有利的介质环境,是导致关中地区地震发生的主要原因。

This study shows that there are 4 kinds of volcanic facies in deep volcanics in north Songliao Basin: eruptive facies, overflow facies, volcanic vent facies and volcanic sedimentary facies. There are 4 volcanic eruption cycles: Huoshiling period, Shahezi period, Yingchengzi period and Quantou period. There are 4 structural evolution stages: north-south accumulation, west-east subduction, uplift mantle and thin crust, alternative open and close. There are 4 kinds of pool-forming patterns:(1) pattern with the migration along the unconformity and fault to the near crater;(2) pattern with the migration along unconformity and fault to the rift margin;(3) pattern with the migration along unconformity, fault and fracture to the source rock;(4) pattern with the migration of the deep gas along the deep and large fault to the volcanic trap.

研究认为,松辽盆地北部深层火山岩主要存在四种火山岩相:即爆发相、溢流相、火山通道相、火山沉积相,划分为四个火山喷发旋回:即火石岭期、沙河子期、营城子期、泉头期,经历了四个构造演化过程:即南北夹攻、东西俯冲、幔隆壳薄、开合交替,具有四种成藏模式:即沿不整合面和断层运移至近火山口处火山岩圈闭聚集成藏模式、沿不整合面和断层砂岩疏导层运移至断陷边部火山岩圈闭聚集成藏模式、沿不整合面及断层、裂缝运移至源岩区内凹中隆火山岩圈闭聚集成藏模式、深部无机成因天然气沿深大断裂运移至火山岩圈闭聚集成藏模式。

The Earth crust activity of different geotectonic elements could be estimated with the fracture fractal dimension.

利用断裂尺度分布的分形维数值的大小,可以定性判断不同大地构造单元的地壳稳定性。

The Earth crust activity of different geotectonic elements could he estimated with the fracture fractal dimension.

利用断裂尺度分布的分形维数值的大小,可以定性判断不同大地构造单元的地壳稳定性。

A fracture in the continuity of a rock formation caused by a shifting or dislodging of the earth's crust, in which adjacent surfaces are ''.

断层由于地壳的变动或移动而引起的在岩石构成连续性上的破裂,伴之以裂缝的一边相对于另一边的错位

A fracture in the continuity of a rock formation caused by a shifting or dislodging of the earth's crust, in which adjacent surfaces are differentially displaced parallel to the plane of fracture .

断层由于地壳的变动或移动而引起的在岩石构成连续性上的破裂,伴之以裂缝的一边相对于另一边的错位

A fracture in the continuity of a rock formation caused by a shifting or dislodging of the earth's crust,in which adjacent surfaces are differentially displace d parallel to the plane of fracture.

断层由于地壳的变动或移动而引起的在岩石构成连续性上的破裂,伴之以裂缝的一边相对于另一边的错位

With the application of the RFPA(superscript 3D)-Parallel system to simulate the fracture spacing phenomenon in the medium of earth crust, failure process and fracture evolution in heterogeneous medium like rock are revealed: and it indicates the broad potential application of the system.

应用RFPA(上标 3D)-Parallel并行分析系统模拟地壳介质中广泛存在的龟裂现象,再现非均匀介质破坏和裂纹演化过程,从而显示该系统广泛的应用前景。

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