...
首页> 外文期刊>Earthquake Research in China >Change of wave velocity in fault regions before the instability of frictional sliding of rocks
【24h】

Change of wave velocity in fault regions before the instability of frictional sliding of rocks

机译:岩石摩擦滑动失稳前断层区域波速的变化

获取原文
获取原文并翻译 | 示例
           

摘要

The experimental study of the change of wave velocity in fault regions before instability of frictional sliding of rocks was conducted. Experiments show that before the instability of frictional sliding of rocks, the change of wave velocity cannot be observed along lines on one side of the fault, but the precursor of the decrease of wave velocity can be observed along lines across the fault. Therefore, when we try to predict the earthquakes of the stick-slip type in fault regions by using the anomaly of wave velocity, the measuring lines across the faults should be selected.
机译:进行了岩石摩擦滑动失稳前断层区域波速变化的实验研究。实验表明,在岩石摩擦滑动失稳之前,不能沿着断层一侧的线观察到波速的变化,但是可以沿着断层两侧的线观察到波速下降的前兆。因此,当我们试图利用波速的异常来预测断层区域的粘滑型地震时,应选择跨断层的测量线。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号