中国东南地区强震活动的对偶现象
DOI:
作者:
作者单位:

作者简介:

通讯作者:

基金项目:


A DUAL PHENOMENON OF STRONG SHOCK ACTION IN SOUTHEAST CHINA
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
    摘要:

    中国东南地区,强震(M≥4(3)/(4)级)往往在一个断裂带中呈对偶活动,它们和构造形状申的斜方式和单斜式的对称性一样,反映了应力作用和地壳运动的对称性,但由于影响发震过程的有关因素的差异,对偶的两次地震的震级差为0-1级,间隔时间为几个月至近百年,震中间距为15-300公里,而这些参数又与本区的具体条件密切相关。自公元1500-1977年期间,本区强震的对偶活动占所发生强震次数的61%,它具有一定的普遍性,因此在地震预报中具有一定的参考价值。

    Abstract:

    In Southeast China, strong shocks(M≥4(3)/(4)) often present dual activities along a fault zone.Along with the symmetric feature of rhombic and monoclinal types in geological structure, it reflects the symmetric feature of tectonic stress and crust movement. Because of the difference of some factors which affects the process of earthquake occurring, the difference between magnitudes of the two earthquakes in pairs reaches 0-1 M, the interval is from several months to near hundred years, and the distance of epicenters is 15-300km. These parameters are closely related to the regional concrete conditions.
    The strong shocks occurred in pairs make up 61 per cent of the total strong shocks in this region, during 1500-1977, it indicates that it has rather an universal feature that the earthquakes often occur in pairs. Therefore, the discovery is useful for earthquake prediction.

    参考文献
    相似文献
    引证文献
引用本文

谢广林.中国东南地区强震活动的对偶现象[J].地震工程学报,1983,5(1):60-65. Xie Guang-lin. A DUAL PHENOMENON OF STRONG SHOCK ACTION IN SOUTHEAST CHINA[J]. China Earthquake Engineering Journal,1983,5(1):60-65.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
历史
  • 收稿日期:1980-06-20
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期: 2017-06-24