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pro vyhledávání: '"Skourtsos, E"'
Akademický článek
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Cephalonia, located in the middle of the central Ionian Islands, has been affected by destructive earthquakes during both the instrumental and the historical period. Despite the fact that it is widely studied from several scientific viewpoints, limit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::201834ce7f5a02e4dae8e6ca86729470
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3219199
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3219199
Our current understanding on sedimentary deep-water environments is mainly built of information obtained from tectonic settings such as passive margins and foreland basins. More observations from extensional settings are particularly needed in order
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::890c37c6d854f6551f7407212574bee7
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3068649
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3068649
Autor:
Muravchik, Martin, Henstra, Gijs Allard, Eliassen, Gauti, Gawthorpe, Rob, Leeder, MR, Kranis, H, Skourtsos, E, Andrews, J.
Externí odkaz:
https://hdl.handle.net/1956/22946
On June 12, 2017, an Mw 6.3 earthquake struck Lesvos Island (Northeastern Aegean, Greece). Building damage was observed in its southeastern part with very heavy structural damage limited in the settlement of Vrissa. Taking into account that Vrissa is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::42e9cb381638f1e2a145c9140d70e0cf
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3060145
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3060145
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
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The onshore central Corinth rift contains a syn-rift succession >3 km thick deposited in 5–15 km-wide tilt blocks, all now inactive, uplifted and deeply incised. This part of the rift records upward deepening from fluviatile to lake-margin conditio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::7f04bebcc7c483ec52c65cd748baabcd
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069229
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069229
Mt Chelmos in the Peloponnesus was glaciated by a plateau ice field during the most extensive Pleistocene glaciation. Valley glaciers radiated out from an ice field over the central plateau of the massif. The largest glaciations are likely to be Midd
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::73b647ae5f0c198c5adba6bf398fcfd7
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3035798
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3035798
Autor:
Papadimitriou, P., Tselentis, G.A., Voulgaris, N., Kouskouna, V., Lagios, E., Kassaras, I., Kaviris, G., Pavlou, K., Sakkas, V., Moumoulidou, A., Karakonstantis, A., Kapetanidis, V., Sakkas, G., Kazantzidou, D., Aspiotis, T., Fountoulakis, I., Millas, C., Spingos, I., Lekkas, E., Antoniou, V., Mavroulis, S., Skourtsos, E., Andreadakis, E.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6210f2e80faa8e1dfec5a6a8728677df