近代地球动力学中的参数效应

IF 1 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Yu. O. Kuzmin
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引用次数: 0

摘要

摘要:本文讨论了近代地球动力学中的参数效应,即断裂带的异常变形过程发生在区域准静态应力的背景下,并且是由小的自然和人为影响引起的断裂带内部介质参数的波动引起的。介绍了岩石试样在长期(1年)单轴准静态加载下参数变形的物理模拟结果。杨氏模量的变化周期为0.03-0.3年,伴随着岩石样品电位的变化。给出了堪察加强震准备过程在断裂带中诱发参数变形形成的实例。给出了气象因素对地表局部变形影响的估计。结果表明,在线性加载情况下,温度日变化和年变化的影响最大。在断裂带过程的非线性参数激励下,最大变形是由降雨引起的。指出了G.A.索博列夫对发展由小的自然撞击引起的地球表面局部变形的研究的贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Parametric Effects in Recent Geodynamics

Parametric Effects in Recent Geodynamics

Abstract—The article discusses parametric effects in recent geodynamics, when anomalous deformation processes in fault zones occur in the setting of regional quasistatic stresses and are caused by fluctuations in the parameters of the medium inside the fault zones themselves, induced by small natural and man-made impacts. The results of physical modeling of parametric deformations under long-term (1 year) uniaxial quasistatic loading of rock samples are presented. Changes in Young’s modulus with periods of 0.03–0.3 years, accompanied by variations in the electrical potentials of rock samples, are revealed. Examples of the formation of parametric deformations induced in the fault zones by the process of preparation of a strong earthquake in Kamchatka are shown. Estimates of the influence of meteorological factors on local deformations of the ground surface are given. It is shown that in the case of linear loading , diurnal and annual temperature variations have the greatest influence. Under nonlinear parametric excitation of the processes in the fault zones, maximum deformations are caused by rainfall. The contribution of G.A. Sobolev to the development of studies of local deformations of the Earth’s surface induced by small natural impacts is noted.

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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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