Abstract
The paper analyzes the possibility of extracting a geophysical field component from a time series considered as a phase projection of a dynamic system. Based on model calculations, the method of averaging of phase trajectories is shown to be applicable for the recovery of time variations of a dynamic system and more reliable determination of its quantitative characteristics if the variations are superimposed by a high-dimension process (a purely random process) and a low-dimension process (linear interpolation). The analysis of the extraction of dynamic system variations from strain records obtained at various points of seismically active regions of China provided the following estimates of dynamic parameters: the phase space dimension is m = 5–7, and the correlation dimension varies, depending on the observation point, within the range d 2 = 2.6–3.5.
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Original Russian Text © A.S. Cherepantsev, 2008, published in Fizika Zemli, 2008, No. 2, pp. 39–58.
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Cherepantsev, A.S. Determination of the phase projection of a dynamic system from strain field observations. Izv., Phys. Solid Earth 44, 119–137 (2008). https://doi.org/10.1134/S106935130802002X
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DOI: https://doi.org/10.1134/S106935130802002X