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弹性回跳模型:从经典走向未来
  • ISSN号:0253-4967
  • 期刊名称:地震地质
  • 时间:2014.9.15
  • 页码:825-832
  • 分类:P316[天文地球—地震学;天文地球—固体地球物理学;天文地球—地球物理学]
  • 作者机构:[1]中国地震局地质研究所、地震动力学国家重点实验室,100029
  • 相关基金:国家自然科学基金“断层失稳滑动观测与瞬态过程分析”项目(41174046)资助.
  • 相关项目:断层失稳滑动观测与瞬态过程分析
作者: 刘力强|
中文摘要:

弹性回跳模型包含3个基本要点:1)地震来自于断层的运动;2)断层运动导致其两侧的岩石发生不均匀的弹性变形,积累巨大的能量,地震中部分弹性能得以释放;3)在断层带的各个点上积累能量的过程是缓慢而不均匀的.Brace(1966)提出弹性回跳的物理机制应当用摩擦滑动过程中出现的不平稳滑动(jerky sliding motion或stick-slip)来解释.Byerlee定律以量化形式表达了地壳摩擦规律,但是没有给出变差的范围.用弹簧滑块模型比拟粘滑,摩擦单元被抽象为刚性滑块,变形被归结于实验加载机的机械框架.后人在此基础上发展了所谓的速度依赖性模型.实验结果表明,速度扰动所带来的摩擦系数变化远远小于材料本身摩擦系数波动,其影响儿乎可以忽略不计.而刚性摩擦滑块的假定与实验观测不符,本质上违反了弹性回跳模型所描述的地震现场考察结果.回到经典就是回归对地震现场问题的研究,这是正确的未来之路.

英文摘要:

After the great 1906 San Francisco earthquake,in 1910,Harry Fielding Reid published the article "The Mechanics of the Earthquake".From an investigation of the deformation of the ground surface which accompanied the 1906 earthquake and the seismological data from USGS Reid expounded explicitly the correlation between the faults and the shallow earthquake.He put forward firstly the elastic rebound model to explain the mechanical mechanism of the earthquake.The model consists of three basic points:1) The earthquake originates from the fault movement; 2)The movement leads to the inhomogeneous elastic deformation on both sides of fault,accumulating vast amounts of energy; 3) Part of the elastic energy is released in the earthquake.Brace(1966) proposed that the physical mechanism of elastic rebound should be explained with jerky sliding motion or stick-slip which is well-known in engineering.The introduction of the stick-slip concept combines the physical interpretation of the earthquakes between the shallow and deep source one and converts the research of deformation into the problem of friction,thus,resulting in a great upsurge in the study of friction in the 1970s to 90s.Twelve years later,Byerlee published the research paper-Friction of rock(1978),regarded as the Byerlee’s Law,that is,when the normal stress σn is smaller than 2kb,the shear stress τ =0.85σn approximately ; when σn is larger than 2kb,τ =0.5 + 0.65σn.Unfortunately,although Byerlee’s paper referred to the variation of data for many times,the empirical formula of his own did not give the range of variation,so the reader could not calculate or evaluate its reliability.Furthermore,in the friction constitutive relation expressed by a piecewise function,the cut-off point is set at 2kb,of which there have been no explanations about its physical meaning or statistical basis so far.In Byerlee’s frame,stick-slip is assimilated as a spring-block model.Fault displacement is set for the rigid block friction movement and deformatio

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期刊信息
  • 《地震地质》
  • 北大核心期刊(2011版)
  • 主管单位:中国地震局
  • 主办单位:中国地震局地质研究所
  • 主编:邓起东
  • 地址:北京市朝阳区华严里甲一号
  • 邮编:100029
  • 邮箱:dzdz@ies.ac.cn
  • 电话:010-62009049
  • 国际标准刊号:ISSN:0253-4967
  • 国内统一刊号:ISSN:11-2192/P
  • 邮发代号:82-809
  • 获奖情况:
  • 1992年被评为全国优秀期刊三等奖,1992年被评为北京市优秀科技期刊四通奖,1992年荣获国家地震局首次科技期刊评比三等奖,1996年荣获国家地震局第二届科技期刊评比二等奖,1997年荣获第二届全国优秀科技期刊评比三等奖,2001年进入中国期刊方阵,被评为“双效”期刊,2009年在中国地震学会组织的地震局系统优秀期刊评...
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  • 被引量:9707