Introduction
Earthquake prediction remains one of the most challenging problems in geoscience. Traditional methods primarily rely on monitoring crustal physical parameters (such as crustal stress, geoelectricity, geomagnetism, groundwater levels). However, these parameters are often highly localized and susceptible to numerous interference factors, making it difficult to establish universal...
I. Theoretical Basis and Physical Mechanisms
1.1 Topological Vortex Stress Field:
The time-varying angle between the Earth's rotation axis and the Sun's rotation axis (e.g., nutation, precession) can, through angular momentum conservation and gravitational torque, form a vortex-like stress field within the Earth's interior, inducing minor crustal deformations. This deformation manifests as...
III. Challenges and Validation Requirements
3.1 Data Noise Filtering:
Crustal deformation signals might be masked by interference such as atmospheric disturbances and temperature fluctuations. Extracting the characteristic signatures of topological vortices will likely require advanced data analysis techniques like machine learning.
3.2 Interdisciplinary Validation:
Validation of the causal...
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