Abstract

This paper describes a technique for determining the potential energy of deformed material around a future earthquake rupture, with this energy being stored during the precursory period. The basic parameters are the following: rupture length on the Earth’s surface after the earthquake has occurred , rupture depth h, and the relative block movement along the rupture strike line . We compared the results for 44 large earthquakes with those derived by determining seismic wave energy from earthquake magnitude.

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