Zobrazeno 1 - 10
of 18
pro vyhledávání: '"G. N. Stavrakakis"'
Publikováno v:
Annals of Geophysics, Vol 40, Iss 1 (1997)
The three-dimensional attenuation structure beneath the Aegean sea and the surrounding regions was determined by inversion of seismic intensity data. A large number of seismic intensity data have been accumulated in a uniform scale in the Aegean regi
Externí odkaz:
https://doaj.org/article/bac9be5717a8488ea5d033b1dd41e5d9
Publikováno v:
Annals of Geophysics, Vol 40, Iss 1 (1997)
The magnetotelluric sounding method at 15 sites was employed to investigate the electrical properties of the crust and upper mantle near the epicentral region of the June 15 1995, Ms = 6.1, destructive earthquake in the Gulf of Corinth, Central Greec
Externí odkaz:
https://doaj.org/article/a1fbcdc420c74b77aedc67bfc2ce2b3f
Publikováno v:
Annals of Geophysics, Vol 40, Iss 1 (1997)
The three-dimensional velocity structure of the crust in the Aegean sea and the surrounding regions (34.0º-42.OºN, 19.0ºE-29.0ºE) is investigated by inversion of about 10000 residuals of arrival times of P-wave from local events. The resulting ve
Externí odkaz:
https://doaj.org/article/e55a67060b91411296791b8e9e476343
Autor:
G. N. Stavrakakis, F. M. Mele, G. Karantonis, C. Falcone, G. Drakatos, L. Beranzoli, B. Alessandrini
Publikováno v:
Annals of Geophysics, Vol 40, Iss 1 (1997)
We present a tomographic view of the crust and uppermost mantle beneath the Central Mediterranean area obtained from P-wave arrival times of regional earthquakes selected from the ISC bulletin. The P-wave velocity anomalies are obtained using Thurber
Externí odkaz:
https://doaj.org/article/a25e81d9abfe4459bdbd2d7ab885d24f
Publikováno v:
Physics of the Earth and Planetary Interiors. 130:209-233
Anomalous transient electric signals (ATESs) in the ultra low frequency (ULF) band have been often observed during magnetotelluric (MT) investigations [Nature 319 (1986) 310; Phys. Earth Planet. Int. 114 (1999) 141; Geophys. J. Int. 142 (2000) 948],
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da6f65f9d05950b1e204a59b664862d6
https://doi.org/10.1016/s0031-9201(02)00008-0
https://doi.org/10.1016/s0031-9201(02)00008-0
Publikováno v:
Natural Hazards. 27:47-60
A regional telemetric network of twelve digital broad-band seismic stations has been in full operation since the beginning of 1999, in Greece, operated by the Institute of Geodynamics of the National Observatory of Athens (GI-NOA). On 7 September 199
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56c75042f13f26dd500fe1943ebb0472
https://doi.org/10.1023/a:1019939628612
https://doi.org/10.1023/a:1019939628612
Autor:
G. N. Stavrakakis, G. Chouliaras
Publikováno v:
Journal of Seismology. 5:595-608
Based on previous observations of the phenomenon of precursory seismic quiescence before crustal main shocks and recent results that indicate an increase in the occurrence of main shocks in the next years, we focus this study on the detection of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c827f77747dceda8aac4e03eca26d3dc
https://doi.org/10.1023/a:1012025024887
https://doi.org/10.1023/a:1012025024887
Publikováno v:
Geophysical Journal International. 142:948-969
A deep magnetotelluric sounding (MTS) investigation in the western part of the Gulf of Corinth has revealed a complex electrical image of the crustal structure. The geotectonic structure of the Parnassos unit and the Transition zone in the central He
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8cdc46e2bc8c594a0ac0adee48cd8aa5
https://doi.org/10.1046/j.1365-246x.2000.00226.x
https://doi.org/10.1046/j.1365-246x.2000.00226.x
Publikováno v:
Physics of the Earth and Planetary Interiors. 114:141-163
Claims by the VAN group [Varotsos, P., Alexopoulos, K., 1984. Physical properties of the variations of the electric field of the earth preceding earthquakes, I. Tectonophysics 110, 73–98, and later works] to have developed a short-term earthquake p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea35cc4af8b3d765504697b2833f8fdc
https://doi.org/10.1016/s0031-9201(99)00050-3
https://doi.org/10.1016/s0031-9201(99)00050-3
Publikováno v:
Geophysical Research Letters. 25:2229-2232
The study of electromagnetic noise in the Ioannina region (NW Greece) shows the existence of long transient electric signals (duration>10 s) without measurable correlated magnetic signals, as is the case for Seismic Electric Signal (SES) observed in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8aa7b24d3c1cdb915938f12a6f9cd96
https://doi.org/10.1029/98gl01593
https://doi.org/10.1029/98gl01593