Citation

Vallianatos F, Papadakis G, Michas G. Proc. Math. Phys. Eng. Sci. 2016; 472(2196): e20160497.

Affiliation

UNESCO Chair on Solid Earth Physics and Geohazards Risk Reduction, Laboratory of Geophysics and Seismology , Technological Educational Institute of Crete , Chania , Greece.

Copyright

(Copyright © 2016, The Royal Society)

DOI

10.1098/rspa.2016.0497

PMID

28119548

Abstract

Despite the extreme complexity that characterizes the mechanism of the earthquake generation process, simple empirical scaling relations apply to the collective properties of earthquakes and faults in a variety of tectonic environments and scales. The physical characterization of those properties and the scaling relations that describe them attract a wide scientific interest and are incorporated in the probabilistic forecasting of seismicity in local, regional and planetary scales. Considerable progress has been made in the analysis of the statistical mechanics of earthquakes, which, based on the principle of entropy, can provide a physical rationale to the macroscopic properties frequently observed. The scale-invariant properties, the (multi) fractal structures and the long-range interactions that have been found to characterize fault and earthquake populations have recently led to the consideration of non-extensive statistical mechanics (NESM) as a consistent statistical mechanics framework for the description of seismicity. The consistency between NESM and observations has been demonstrated in a series of publications on seismicity, faulting, rock physics and other fields of geosciences. The aim of this review is to present in a concise manner the fundamental macroscopic properties of earthquakes and faulting and how these can be derived by using the notions of statistical mechanics and NESM, providing further insights into earthquake physics and fault growth processes.

Language: en

Keywords

Tsallis entropy; complexity; earthquakes; faulting; scaling; statistical mechanics