北京地区地壳Q值随深度的分布特征
DOI:
作者:
作者单位:

作者简介:

通讯作者:

基金项目:


THE DISTRIBUTION CHARACTERISTICS OF Q VALUE WITH DEPTH IN THE CRUST IN BEIJING AREA
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:

    地震波在介质中的衰减,是介质的重要特性之一,而Q值则是衡量衰减特性的主要物理参数,称之谓介质的品质因子。根据文献[1]提出的方法,用北京台网记到的近震直达P波资料,测定北京地区的大量Q值表明[2]:Q值与P、S波到时差(ts-tp,)有关,(ts-p)大,测得的Q值也大; (ts-tp)小,测得的Q值也小。

    Abstract:

    In this paper,the method of calculating Q value with depth in the cr-ust by means of data of near earthquakes is described.
    It is found that the relationship Q (z)=26.27z-14.4(z>11Km) may be adopted in Beijing and its adjacent region.The results obtained also show that Q value is 300-400 in the depth from 11-15Km which is the average focal depth in Beijing area,and Q-1000 approaching to the bottom of the crust.

    参考文献
    相似文献
    引证文献
引用本文

付昌洪,朱传镇.北京地区地壳Q值随深度的分布特征[J].地震工程学报,1982,4(4):63-68. Fu Changhong, Zhu Chuanzhen. THE DISTRIBUTION CHARACTERISTICS OF Q VALUE WITH DEPTH IN THE CRUST IN BEIJING AREA[J]. China Earthquake Engineering Journal,1982,4(4):63-68.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期: 2017-07-04