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- > EVELPIDOU, N., (Editeur scientifique) (supprimer)
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Par Collection Par Auteur- EVELPIDOU, N., (Editeur scientifique) (2)
- PAVLOPOULOS, K., (Editeur scientifique) (2)
- BASSIAKOS, Y. (1)
- FOUNTOULIS, I. (1)
- KAROTSIERIS, Z. (1)
- LATOCHA, A. (1)
- MALIK, I. (1)
- MARIOLAKOS, I. (1)
- THEODORAKOPOULOU, K. (1)
- TRIANTAPHYLLOU, M. (1)
- WISTUBA, M. (1)
- ATHANASSAS, C. (1)
- OWCZAREK, P. (1)
- 2013 (2)
- Alud de residuos ; Dendrocronología ; Dendrología ; Formación arbustiva ; Spitzberg ; Zona fría ; Ártica (1)
- Archeological site ; Coastal environment ; Dating ; Geoarchaeology ; Greece ; Marine terrace ; Neotectonics ; Optically stimulated luminescence ; Peloponnese ; Quaternary ; Roman era ; Sea level ; Thermoluminescence (1)
- Cuaternario ; Datación ; Geoarqueología ; Grecia ; Litoral ; Neotectónica ; Nivel del mar ; Peloponeso ; Sitio arqueológico ; Termoluminiscencia ; Terraza marina ; Época romana (1)
- Datation ; Epoque romaine ; Grèce ; Géoarchéologie ; Littoral ; Luminescence stimulée optiquement ; Messinía ; Niveau marin ; Néotectonique ; Pelopónnisos ; Quaternaire ; Site archéologique ; Terrasse marine ; Thermoluminescence (1)
- Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes (2)
- Comments on the neotectonics of the coastal zone of western Messenia based on luminescence dating and geoarchaeological evidence (1)
- Reconstruction of modern debris flow activity in the arctic environment with the use of dwarf shrubs (south-western Spitsbergen) – a new dendrochronological approach (1)
- specimens, the presence reaction wood and scars were evaluated for their potential in temporal reconstructions in geomorphology. The age of shrubs studied indirectly mark the minimal time, which passed since the last episode of debris flow on the studied
- important indicators of coastal displacement. Specifically, Hellenistic and Roman archaeological sites are useful markers of tectonic subsidence and thus they demonstrate localised diversions from the general pattern of uplift.