Zobrazeno 1 - 10
of 51
pro vyhledávání: '"Konstantinos I. Konstantinou"'
Autor:
Dimitrios Giannopoulos, Efthimios Sokos, Konstantinos I. Konstantinou, Athanasios Lois, G-Akis Tselentis
Publikováno v:
Annals of Geophysics, Vol 55, Iss 5 (2013)
On June 8, 2008, at 12:25 GMT, a Mw 6.4 earthquake, the Movri Mountain earthquake, occurred in the area of northwest Peloponnese, western Greece. The epicenter was located in the municipality of Movri, 35 km southwest of Patras. For this study, a cru
Externí odkaz:
https://doaj.org/article/b49ff41cd34b4aa9b3167c40d1abf028
Publikováno v:
Pure and Applied Geophysics. 177:2579-2595
This study performs a reanalysis of the seismicity recorded during the 1996 Gjálp eruption that occurred at NW Vatnajökull, Iceland. The seismicity was recorded by the temporary HOTSPOT network consisting of 30 three-component broadband stations. I
Seismotectonics of SE Aegean inferred from precise relative locations of shallow crustal earthquakes
Publikováno v:
Journal of Seismology. 24:1-22
We relocated the seismicity in SE Aegean that was recorded by both permanent and temporary seismic networks during 2004–2018 in order to investigate its correlation with the active faults in this area. P and S-phase travel times of best quality eve
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:10393-10412
Publikováno v:
Physics of the Earth and Planetary Interiors. 290:99-106
Erebus is an intraplate stratovolcano of phonolitic composition located at the southern end of Terror Rift within the West Antarctica Rift system. The volcanic edifice of Erebus exhibits a summit plateau that hosts the main crater and a smaller inner
Southern Aegean is the major part of the Eurasian plate overriding the subduction of African plate in eastern Mediterranean region. In this study, shallow depth (< 40 km) events recorded by temporary and permanent seismic networks in southern Aegean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4aaab5ad6d32a2c24ce13177b42f1ef5
https://doi.org/10.5194/egusphere-egu2020-4668
https://doi.org/10.5194/egusphere-egu2020-4668
Autor:
Konstantinos I. Konstantinou
Publikováno v:
Journal of Geodynamics. 121:143-154
This study relocates the seismicity in NE Aegean during the period 2011–2017 using data recorded by the Hellenic Unified Seismic Network (HUSN) in order to elucidate the relationship between seismicity and active faults in this area. P- and S-phase
Hazard assessment of volcanic ballistic impacts at Mt Chihshin, Tatun Volcano Group, northern Taiwan
Publikováno v:
Natural Hazards. 92:77-92
This study investigates the hazard posed by Volcanic Ballistic Projectiles (VBPs) in the area surrounding Mt Chihshin, Tatun Volcano Group, northern Taiwan. Based on the volcano’s current evolutionary stage, we consider two types of volcanic activi
Publikováno v:
Pure and Applied Geophysics. 175:731-740
We perform a systematic comparison between local and moment magnitudes in Greece for the period 2008–2016 when both magnitudes have been determined using waveform data recorded by the Hellenic Unified Seismic Network (HUSN). Differences between the
Accurate relocation of seismicity along the North Aegean Trough and its relation to active tectonics
Autor:
Konstantinos I. Konstantinou
Publikováno v:
Tectonophysics. 717:372-382
The tectonics of northern Aegean are affected by the westward push of Anatolia and the gravitational spreading of the Aegean lithosphere that promote transtensional deformation in the area. This regime is also responsible for the creation of a series