基于青藏高原地壳不稳定因素下的引力波地震预测可行性研究

在青藏高原地震是主要破坏性的地质灾害之一,在目前国际社会预测地震的方式主要是利用地震产生的纵横波速差来预测地震,通过阐述人类首次探测到引力波实验原理依据、引力波的产生及其性质、地震的形成机制,分析卫星遥感预测地震的可行性。结果表明地震形成至发生的前夕,大质量物体碰撞或可产生引力波,以波的形成在空间传播引起空间折叠震荡,通过卫星遥感监测或可监测到大面积的空间折叠影像,从而起到预测地震的作用。

Earthquake is one of the main destructive geological disasters in the Qinghai-Tibet Plateau. At present, the way of earthquake prediction in the international community is mainly to use the velocity difference between P-wave and S-wave produced by earthquakes to predict earthquakes. By expounding the experimental basis of the first detection of gravitational waves, the generation and properties of gravitational waves, and the formation mechanism of earthquakes, the feasibility of earthquake prediction by satellite remote sensing is analyzed. The results show that gravitational waves may be produced by the collision of high-mass objects on the eve of the earthquake, and the spatial folding oscillations can be caused by the propagation of waves in space. A large area of spatial folding images can be monitored by satellite remote sensing, which plays a role in earthquake prediction.