一种地震波动应力测算方法、设备、介质及产品

By constructing a method for measuring seismic wave stress, determining the dominant seismic phase and its optimal combination, and using the seismic wave stress formula to calculate the time history of wave stress components, the problem of ineffective measurement of seismic wave stress is solved, and effective measurement and analysis of seismic wave stress is realized.

CN120214892BActive Publication Date: 2026-07-17CHINA UNIV OF GEOSCIENCES (BEIJING) +1

Patent Information

Authority / Receiving Office
CN · China
Patent Type
Patents(China)
Current Assignee / Owner
CHINA UNIV OF GEOSCIENCES (BEIJING)
Filing Date
2025-04-01
Publication Date
2026-07-17

AI Technical Summary

Technical Problem

Existing technologies cannot directly measure the wave stress of seismic waves, especially cannot effectively measure the wave stress of seismic waves.

Method used

A method for calculating seismic wave stress is provided. By constructing a crustal model of the observation area, obtaining measured seismic waves and seismic source mechanism parameters, determining the dominant seismic phase and its optimal combination, calculating the time history of wave stress components using the seismic wave stress formula, and superimposing them in time sequence to obtain the seismic wave stress time history.

Benefits of technology

It enables effective calculation of seismic wave stress, provides calculation methods and equipment for seismic wave stress, can be implemented in a computer, and is suitable for the measurement and analysis of seismic wave stress.

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Abstract

本申请公开了一种地震波动应力测算方法、设备、介质及产品,涉及地震动力学研究技术领域,该方法包括:根据观测区域的地壳结构参数,构建观测区域地壳模型;依据观测区域地壳模型以及与实测地震波对应的地震震源机制,确定观测点处对实测地震波能量贡献显著的卓越震相及其最佳震相组合;利用地震波动应力公式,分别确定每个卓越震相产生的波动应力分量时程;将所有卓越震相产生的波动应力分量时程按到达观测点的时序叠加,得到地震过程在观测点处产生的地震波动应力时程。本申请通过构建观测区域地壳模型确定观测点处实测地震波的最佳震相组合,进而完成地震波动应力测算。
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