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The recent tectonic stress districts and strong earthquakes in China

机译:中国最近的构造应力区和强地震

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摘要

According to the stress state and force source character, the recent tectonic stress field of China is preliminary divided into four classes. Among them, there are two first order districts, four second order districts, five third order districts and twenty-six fourth order districts. By analyzing those tectonic stress districts and strong earthquakes, the close relation between them is mainly summarized as follows: (1) The boundary of stress districts especially the first or second order boundary controlled by the interaction of tectonic plates has strong earthquakes very easily and frequently. (2) Stress districts with stress direction, regime type and stress value transformation are concentrative zones of strong earthquakes. (3) Stress districts with local stress differentiation but in the homogeneous stress background are the places where strong earthquakes are relatively concentrated. On the basis of these research work, we discuss the present dynamic environment in China from force source and plates movement.
机译:根据应力状态和力源特征,将中国近期的构造应力场初步分为四类。其中,有两个一阶区,四个二阶区,五个三阶区和二十六个四阶区。通过分析这些构造应力区与强震之间的密切关系,主要总结如下:(1)应力区的边界,尤其是受构造板块相互作用控制的一,二阶边界,很容易且频繁发生强地震。 。 (2)应力方向,状态类型和应力值转换的应力区是强地震的集中区。 (3)具有局部应力差异但均质应力背景的应力区是强地震相对集中的地方。在这些研究工作的基础上,我们从力源和板块运动的角度讨论了中国目前的动态环境。

著录项

  • 来源
    《Rock stress and earthquakes.》|2010年|p.35-40|共6页
  • 会议地点 Beijng(CN);Beijng(CN)
  • 作者

    Furen Xie; Hongyan Zhang; YiDu;

  • 作者单位

    Institute of Crustal Dynamics, China Earthquake Administration, Beijing, China;

    Institute of Crustal Dynamics, China Earthquake Administration, Beijing, China;

    Institute of Crustal Dynamics, China Earthquake Administration, Beijing, China;

  • 会议组织
  • 原文格式 PDF
  • 正文语种
  • 中图分类 地震学;地震学;地震学;
  • 关键词

  • 入库时间 2022-08-26 14:05:52

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