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Advisor(s)
Abstract(s)
This paper analyses earthquake data in the
perspective of dynamical systems and its Pseudo
Phase Plane representation. The seismic data is collected
from the Bulletin of the International Seismological
Centre. The geological events are characterised
by their magnitude and geographical location and described
by means of time series of sequences of Dirac
impulses. Fifty groups of data series are considered,
according to the Flinn-Engdahl seismic regions of
Earth. For each region, Pearson’s correlation coefficient
is used to find the optimal time delay for reconstructing
the Pseudo Phase Plane. The Pseudo Phase
Plane plots are then analysed and characterised.
Description
Keywords
Pseudo phase plane Pearson’s correlation Optimal time delay Seismic event
