Zobrazeno 1 - 10
of 58
pro vyhledávání: '"M. S. Lazaridou"'
Publikováno v:
Tectonophysics. 589:116-125
Natural time analysis reveals novel dynamical features hidden behind time series in complex systems. By applying it to the time series of earthquakes, we find that the order parameter of seismicity exhibits a unique change approximately at the date(s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40f4c735a8413915680869361029c890
https://doi.org/10.1016/j.tecto.2012.12.020
https://doi.org/10.1016/j.tecto.2012.12.020
Publikováno v:
Proceedings of the Japan Academy. Series B, Physical and Biological Sciences
The behavior of seismicity in the area candidate to suffer a main shock is investigated after the observation of the Seismic Electric Signal activity until the impending mainshock. This makes use of the concept of natural time $��$ and reveals th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c64512a5c7f43364a8f218ec69a8b4eb
https://doi.org/10.2183/pjab.84.331
https://doi.org/10.2183/pjab.84.331
Publikováno v:
Tectonophysics. 412:279-288
Investigating the period 1983–1994 for western Greece, a possible correlation between the selectivity characteristics of the SES (seismic electric signals of the VAN method) and earthquake parameters has been reported by Uyeda et al. [Uyeda, S., Al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0474a8685e2bcd554530ce851b7ae50f
https://doi.org/10.1016/j.tecto.2005.10.037
https://doi.org/10.1016/j.tecto.2005.10.037
Publikováno v:
Geophysical Research Letters. 26:3245-3248
Numerical solutions of Maxwell equations for a model earth with a reasonably conducting channel indicate that the electric field values are intensified within a certain region only (i.e., above the end of the channel), thus explaining the observed se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::750a5a9f00b12a25c163b11ecf74f514
https://doi.org/10.1029/1998gl005265
https://doi.org/10.1029/1998gl005265
Autor:
Konstantinos Eftaxias, N. V. Sarlis, M. S. Lazaridou, Panayiotis A. Varotsos, V. Hadjicontis, N. Bogris
Publikováno v:
Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy. 24:111-114
A Special Issue (Geophys. Res. Lett. 23, 1996) was focused on the question whether the VAN predictions outperform random chance. The majority of the participants of this Debate was selected to be critics against VAN, but Varotsos and co-workers accep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8301327d9d14381c360711466b78d767
https://doi.org/10.1016/s1464-1895(99)00005-8
https://doi.org/10.1016/s1464-1895(99)00005-8
Autor:
A. Abdulla, M. S. Lazaridou, N. V. Sarlis, N. Bogris, P. Kapiris, John P. Makris, Konstantinos Eftaxias, Panayiotis A. Varotsos
Publikováno v:
Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy. 24:115-121
Seismic Electric Signals (SES) were recorded by VAN-group on April 18–19, 1995, at Ioannina station; they resulted in an official prediction that was sent (two weeks before the earthquake occurrence) to the Greek authorities as well as to various I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ab177450ce4042f71414b37c3967f024
https://doi.org/10.1016/s1464-1895(99)00006-x
https://doi.org/10.1016/s1464-1895(99)00006-x
Publikováno v:
Journal of Applied Physics. 83:60-70
The conditions under which pressure (stress) variations on solids, containing charged defects, can lead to the emission of transient electric signals, are discussed. The resulting electric field E varies as 1/d3 (where d denotes the distance from the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0079e8c6b3f720dfccec68c6ffb865f
https://doi.org/10.1063/1.366702
https://doi.org/10.1063/1.366702
Publikováno v:
Geophysical Research Letters. 23:1295-1298
A three year continuous sample of earthquake predictions based on the observation of Seismic Electric Signals in Greece was published by Varotsos and Lazaridou [1991]. Four independent studies analyzed this sample and concluded that the success rate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f1d732a1c469f32bcd5adbd67065450
https://doi.org/10.1029/96gl00905
https://doi.org/10.1029/96gl00905
Publikováno v:
Geophysical Research Letters. 23:1359-1362
Drakopoulos and Stavrakakis [1996] -hereafter called DS- select in their discussion one public alarm (issued on January 1991), but delete three other such cases (issued on Sept. 1988, April 1990 and Febr.–March 1993) which were followed by destruct
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f1e018dd2f7f187c764893be1afa146
https://doi.org/10.1029/96gl00911
https://doi.org/10.1029/96gl00911
Publikováno v:
Geophysical Research Letters. 23:1375-1378
Rhoades and Evison [1996] indicated a technical flaw in the procedure of Mulargia and Gasperini [1992] and also made many useful remarks and fundamental suggestions on the correct way for performing a statistical evaluation of an earthquake predictio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc3f9a06316f2c49f1b70019814bc78b
https://doi.org/10.1029/96gl00910
https://doi.org/10.1029/96gl00910