地震体积的体波研究

1. Institut für Geophysik, Universität Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany;
2. Department of Geophysics, Charles University, Ke Karlovu 3, 12116 Prague, Czech Republic

基金项目:

Supported, in part, by Grant No: 205/07/0502 of the Grant Agency of the Czech Republic

详细信息

The Earthquake Volume from Body Waves

1. Institut für Geophysik, Universität Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany;
2. Department of Geophysics, Charles University, Ke Karlovu 3, 12116 Prague 2, Czech Republic

Funds:

Supported, in part, by Grant No: 205/07/0502 of the Grant Agency of the Czech Republic

摘要: 在地球内部的大部分区域地震体波的传播是线弹性过程,仅在震源周围区域由于波的辐射和传播效应可能导致非线性。本研究主要涉及对非线性过程占优势区域的尺度估计。
- 体波 /
- 应变 /
- 体积
Abstract: The propagation of seismic body waves is a linearly elastic process in most of the Earth body.Only in the region surrounding the earthquake focus nonlinear processes may be expected to take place as the result of the radiation and propagation of the waves.The investigation is concerned with the estimation of the dimension of the region in which nonlinear processes prevail.
- body waves /
- strain /
- earthquake volume