Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Diamantina Griva"'
Autor:
Efthimios Karymbalis, Konstantinos Tsanakas, Diamantina Griva, Dimitrios-Vasileios Batzakis, Kanella Valkanou
The present study is a geomorphological overview of Greece on a scale of 1:1,000,000. It is the first attempt of a cartographic synthesis that aims to bring together and interpret the geological and geomorphological factors that contributed to the la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f0a6d9e98fa6e2c0c4a6eb2d0436931
https://doi.org/10.5194/icg2022-367
https://doi.org/10.5194/icg2022-367
Autor:
Konstantinos Tsanakas, Julius Jara-Muñoz, Efthimios Karymbalis, Cengiz Yildirim, Kevin Pedoja, Dimitrios-Vasileios Batzakis, Diamantina Griva
Offshore islands may furnish valuable information regarding deformation rates, their controlling mechanisms, and the dynamics of the upper crust in offshore areas along subduction zones, which otherwise would be difficult to quantify by direct observ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4ed11d9997b3ddd90ae28a403ba3fe5
https://doi.org/10.5194/icg2022-369
https://doi.org/10.5194/icg2022-369
Autor:
Diamantina Griva, Efthimios Karymbalis, Maurizio Poscolieri, Isaak Parcharidis, Vasilios Kapsimalis, Konstantinos Tsanakas, Dimitrios-Vasileios Batzakis
A beach ridge is a coastal depositional landform defined as a relict shore ridge that is more or less parallel with the coastline and with other landward-adjacent ridges. It is built by wave swash that may be surmounted by wind-deposited sediments. O
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f84c51ea6c2ca2b2ee5b7219cf13704
https://doi.org/10.5194/icg2022-365
https://doi.org/10.5194/icg2022-365
Autor:
Julius Jara-Muñoz, Konstantinos Tsanakas, Efthymios Karymbalis, Cengiz Yildirim, Kevin Pedoja, Dimitrios- Vasileios Batzakis, Diamantina Griva
The coastal morphology of islands may furnish valuable information regarding deformation rates, their controlling mechanisms and the dynamics of the upper crust in offshore areas along subduction zones. Here we study active deformation and faulting a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2533340b2bd40423a25e4e96b804a395
https://doi.org/10.5194/egusphere-egu22-11349
https://doi.org/10.5194/egusphere-egu22-11349