Short-time stress-propagation on the regional and/or planetary scale - Acoustic Emission and other geophysical evidences

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Scientific paper

We emphasise that large regions, of size comparable to a continent, can eventually, or maybe almost permanently, experience a continuous temporal evolution of crustal stress. Such effects, which have close geodynamic implications, can be effectively monitored by some dense array of Acoustic Emission (AE) sensors. They ought to result correlated with other geophysical inferences, such as sea-level variation, GPS monitoring of continental drift, and seismic and/or volcanic activity. A case history is discussed dealing with the Mediterranean basin and with the central Atlantic Ocean, although the AE database is limited to records collected at two sites alone, one in central Italy and one on Vesuvius.

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