Seismicity Variations in the Southern Aegean, Greece, Before and After the Large (M7.7) 1956 Amorgos Earthquake Due to Evolving Stress

@article{Papadimitriou2005SeismicityVI,
  title={Seismicity Variations in the Southern Aegean, Greece, Before and After the Large (M7.7) 1956 Amorgos Earthquake Due to Evolving Stress},
  author={Eleftheria E. Papadimitriou and Georgios Sourlas and Vassilios Karakostas},
  journal={pure and applied geophysics},
  year={2005},
  volume={162},
  pages={783-804}
}
Abstract.The largest earthquake (M0=4.9·1027 dyn·cm) of the 20th century in the territory of Greece occurred south of Amorgos Island, causing extensive destruction in the southern Aegean area. It occurred on an ENE–trending normal fault that is seated parallel to the Island’s southern coastline. Changes in the rates of moderate–size earthquakes (M ≥ 5.0) that occurred before and after the Amorgos earthquake, within circular regions centered on its epicenter with radii of 100, 150 and 200 km… 

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