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On Determining of the Ultimate Strain of Earth Crust Rocks by the Value of Relative Slips on the Earth Surface After a Large Earthquake

机译:大地震后地表相对滑移值确定地壳岩石的极限应变

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The value of the Earth crust rocks ultimate strain together with other physical-and-mechanical characteristics plays an important role in problems on setting maximal values of displacements, velocities and accelerations of grounds in the course of quakes, in determining of the value of potential strain energy accumulated in the medium when a process of a large quake maturation runs, in prognostication of a quake by "ultimate strain of rocks" forerunner as well as other problems, are related to the soil bearing resistance and behaviour. The paper represents a developed method for determining the magnitude of ultimate strain of soils thickness of the Earth crust in natural conditions by the relative slips on the earth surface after a large earthquake. Are obtained the empirical dependences of the value of ultimate strain from magnitude of earthquake, relative slips, the rupture length, and seismic moment by analysing values calculated by the proposed method for the 44 strong earthquakes with a magnitude of 5.6-8.5. A comparative analysis of the ultimate strain values is given which is obtained by other authors by the method of geodesic triangulation.
机译:地壳岩石极限应变的值以及其他物理和机械特性在设定地震过程中地面位移,速度和加速度的最大值,确定潜在应变值的问题中起着重要作用。当大地震成熟过程进行时,在介质中积累的能量,通过“终极岩石应变”先兆预后的地震以及其他问题,都与土壤的承载力和行为有关。本文代表了一种确定的方法,该方法可通过大地震后地表上的相对滑动来确定自然条件下地壳土壤厚度的极限应变大小。通过分析针对44个5.6-8.5级强地震的建议方法计算出的值,获得了极限应变值与地震强度,相对滑动,破裂长度和地震矩的经验相关性。给出了最终应变值的比较分析,这是由其他作者通过测地线三角剖分法获得的。

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