The seismotectonic regime in Greece

Evidence is presented which favours the theory that the<br />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 Southeaste...

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Bibliographic Details
Main Author: GALANOPOULOS A. G.
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1967-06-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4987
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spelling doaj-f9d8651660794eb5be70a9e5ece60c7e2020-11-25T00:52:40ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1967-06-0120110911910.4401/ag-4987The seismotectonic regime in GreeceGALANOPOULOS A. G.Evidence is presented which favours the theory that the<br />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.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4987
collection DOAJ
language English
format Article
sources DOAJ
author GALANOPOULOS A. G.
spellingShingle GALANOPOULOS A. G.
The seismotectonic regime in Greece
Annals of Geophysics
author_facet GALANOPOULOS A. G.
author_sort GALANOPOULOS A. G.
title The seismotectonic regime in Greece
title_short The seismotectonic regime in Greece
title_full The seismotectonic regime in Greece
title_fullStr The seismotectonic regime in Greece
title_full_unstemmed The seismotectonic regime in Greece
title_sort seismotectonic regime in greece
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1967-06-01
description Evidence is presented which favours the theory that the<br />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.
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4987
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