18 citations as recorded by crossref.

1. The 2025 South Aegean Sea Seismic Swarm Activity in Natural Time and the Generalized Gutenberg–Richter Law N. Sarlis et al. https://doi.org/10.3390/app16146859
2. Landslide Induced Tsunami Hazard at Volcanoes: the Case of Santorini O. Necmioglu et al. https://doi.org/10.1007/s00024-023-03252-8
3. Focal mechanism and depth of the 1956 Amorgos twin earthquakes from waveform matching of analogue seismograms A. Brüstle et al. https://doi.org/10.5194/se-5-1027-2014
4. Operational network improvements and increased reporting in the NOA (Greece) seismicity catalog G. Chouliaras et al. https://doi.org/10.5194/adgeo-36-7-2013
5. Stress distribution and seismicity patterns of the 2011 seismic swarm in the Messinia basin, (South-Western Peloponnesus), Greece G. Chouliaras et al. https://doi.org/10.5194/nhess-13-45-2013
6. Empirical seismic vulnerability, deterministic risk and monetary loss assessment in Fira (Santorini, Greece) D. Kazantzidou-Firtinidou et al. https://doi.org/10.1007/s11069-018-3350-8
7. The Santorini Volcanic Complex: A detailed multi-parameter seismological approach with emphasis on the 2011–2012 unrest period P. Papadimitriou et al. https://doi.org/10.1016/j.jog.2014.12.004
8. Oceanographic Signatures and Pressure Monitoring of Seafloor Vertical Deformation in Near-coastal, Shallow Water Areas: A Case Study from Santorini Caldera G. Vilaseca et al. https://doi.org/10.1080/01490419.2016.1226222
9. A detailed seismic anisotropy study during the 2011–2012 unrest period in the Santorini Volcanic Complex G. Kaviris et al. https://doi.org/10.1016/j.pepi.2014.11.002
10. Seismicity, Vp/Vs and shear wave anisotropy variations during the 2011 unrest at Santorini caldera, southern Aegean K. Konstantinou et al. https://doi.org/10.1016/j.jvolgeores.2013.10.001
11. Evidence of non-extensivity in the seismicity observed during the 2011–2012 unrest at the Santorini volcanic complex, Greece F. Vallianatos et al. https://doi.org/10.5194/nhess-13-177-2013
12. Seismicity patterns and b-value variability in the Santorini–Amorgos system within the South Aegean volcanic arc G. Polat & G. Altın https://doi.org/10.1007/s11600-026-02007-y
13. Characterising the 2025 Santorini–Amorgos seismic swarm: Implications of magmatic and tectonic processes K. Lentas et al. https://doi.org/10.1016/j.tecto.2026.231125
14. SqueeSAR™ and GPS ground deformation monitoring of Santorini Volcano (1992–2012): Tectonic implications E. Lagios et al. https://doi.org/10.1016/j.tecto.2013.03.012
15. Relationship Between Dike Injection and b‐Value for Volcanic Earthquake Swarms A. Glazner & S. McNutt https://doi.org/10.1029/2020JB021631
16. The initiation and development of a caldera-forming Plinian eruption (172 ka Lower Pumice 2 eruption, Santorini, Greece) J. Simmons et al. https://doi.org/10.1016/j.jvolgeores.2017.05.034
17. Spatial and Magnitude Distribution of Seismic Events in Santorini Island, January–February 2025: Tectonic or Volcanic Earthquakes? A. Moshou https://doi.org/10.3390/geohazards6040081
18. Extensional tectonics and magma-driven seismicity across the Santorini–Amorgos basins, south-central Aegean Sea: insights from the 2025 earthquake swarm S. Yolsal-Çevikbilen et al. https://doi.org/10.1093/gji/ggag394