The seismotectonic regime in Greece

GALANOPOULOS A. G.

Abstract


Evidence is presented which favours the theory that the
earthquake activity in the area of Greece should bo ascribed to horizontal currents flowing off to the side of the secondary sedimentary arc, from a minor mantle current rising under the primary volcanic arc of the Southeastern section of the Dinaric Alps.

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References


DOI: https://doi.org/10.4401/ag-4987
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Published by INGV, Istituto Nazionale di Geofisica e Vulcanologia - ISSN: 2037-416X