Fault architecture, basin structure and evolution of the Gulf of Corinth Rift, central Greece
The style of extension and strain distribution during the early stages of intra‐continental
rifting is important for understanding rift‐margin development and can provide constraints for …
rifting is important for understanding rift‐margin development and can provide constraints for …
Mid-miocene to recent tectonic evolution of the punta stilo swell (calabrian arc, southern Italy): an effect of calabrian arc migration
Abstract The development of Punta Stilo Swell (PSS), a submerged lobate-shaped
promontory located in the Crotone-Spartivento Basin, is inferred to be closely linked to the …
promontory located in the Crotone-Spartivento Basin, is inferred to be closely linked to the …
Scaling properties within the Gulf of Corinth, Greece; comparison between offshore and onshore active faults
The Gulf of Corinth, Greece, is a 110-km-long by 30-km-wide active graben displaying
strong seismicity hosted both on north and south dipping normal faults. This complex fault …
strong seismicity hosted both on north and south dipping normal faults. This complex fault …
Morphological variability of submarine mass movements in the tectonically–controlled Calabro–Tyrrhenian Continental Margin (Southern Italy)
The analysis of high resolution morpho–bathymetric data on the Calabro Tyrrhenian
continental margin (Southern Italy) enabled us to identify several morphological features …
continental margin (Southern Italy) enabled us to identify several morphological features …
[PDF][PDF] Returning to the facts: Response to the refusal of tsunami traces in the ancient harbour of Lechaion (Gulf of Corinth, Greece) by 'non-catastrophists'–Reaffirmed …
The ancient harbour of Lechaion supposedly was one of the most important harbours of the
ancient world. Representing the western harbour of Corinth at the eastern end of the Gulf of …
ancient world. Representing the western harbour of Corinth at the eastern end of the Gulf of …
Geomorphological Analysis of Xilokastro Fault, Central Gulf of Corinth, Greece
S Verroios, V Zygouri - Geosciences, 2021 - mdpi.com
The Gulf of Corinth is a rapidly opening area with high seismicity associated with extensive
building collapses, destruction of cities, and even the deaths of inhabitants. Rapid …
building collapses, destruction of cities, and even the deaths of inhabitants. Rapid …
[PDF][PDF] Ancient Greek harbours used as geo-archives for palaeotsunami research: case studies from Krane (Cefalonia), Lechaion (Gulf of Corinth) and Kyllini …
H Hadler - 2014 - openscience.ub.uni-mainz.de
Since historical times, coastal areas throughout the eastern Mediterranean are exposed to
tsunami hazard. For many decades the knowledge about palaeotsunamis was solely based …
tsunami hazard. For many decades the knowledge about palaeotsunamis was solely based …
[PDF][PDF] Returning to the facts: Response to the refusal of tsunami traces in the ancient harbour of lechaion (Gulf of Corinth, Greece) by'non-catastrophists'-Reaffirmed …
A VOtt, H Hadler, B Koster… - Zeitschrift fur …, 2018 - academia.edu
The ancient harbour of Lechaion supposedly was one of the most important harbours of the
ancient world. Representing the western harbour of Corinth at the eastern end of the Gulf of …
ancient world. Representing the western harbour of Corinth at the eastern end of the Gulf of …
[PDF][PDF] Fault reactivation and its effects on the petroleum systems of continental margins
N Mattos - 2017 - core.ac.uk
This research project uses high-quality seismic data from the Ottar Basin offshore Norway,
Espírito Santo Basin offshore Brazil and Taranaki Basin offshore New Zealand. It …
Espírito Santo Basin offshore Brazil and Taranaki Basin offshore New Zealand. It …
Late Quaternary sedimentation in the western tip of the Gulf of Corinth: Interplay between tectonic deformation, seismicity and eustatic changes
A Beckers - 2015 - search.proquest.com
Abstract The Corinth Rift, Greece, is a young and active continental rift stretching over~ 150
km between the cities of Patras and Athens. The most active part of the rift, where the …
km between the cities of Patras and Athens. The most active part of the rift, where the …