Citation

Teramo A, Termini D, Stillitani E, Bottari A. Nat. Hazards 1996; 13(2): 101-117.

Copyright

(Copyright © 1996, Holtzbrinck Springer Nature Publishing Group)

DOI

10.1007/BF00138478

PMID

unavailable

Abstract

A vectorial modelling of observed macroseismic intensity aimed at the analytical determination of the epicentre is proposed here. The methodology is based on the determination of a plane system of vectors which characterises the macroseismic intensity distribution. The epicentre of each seismic event considered is determined as the centre of this vector system by an analytical expression which is independent from all possible directions of seismic energy propagation. The analysis of the intensity distribution is carried out by a new model called a macroseismic plane, different from the one known as macroseismic field, formed by a set of small areas built around the observed intensity points; hence its name. With the proposed methodology, some earthquakes in southern Italy and eastern Sicily are analysed calculating their epicentres, also for distributions of observed intensity which are particularly complex.

Language: en