EGU General Assembly 2007
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  Oral Programme - NH4.03 Deformation processes and accompanying mechanical and electromagnetic phenomena, for rocks and other materials, from the laboratory to the geophysical scale

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Convener: Eftaxias, K.
Co-Convener: Chelidze, T., Morgounov, V., Nomicos, C., Mandea, M.

Thursday, 19 April 2007

Lecture Room: Lecture Room 16 (L)

Chairperson: MANDEA , M.

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8:30 - 9:00
EGU2007-A-00442;  NH4.03-1TH1O-001
Chelidze, T.; Lursmanashvili, O.; Matcharashvili, T.
Electromagnetic Forcing of Stick-Slip Deformation: multiple synchronization and phase shift (solicited)

9:00 - 9:30
EGU2007-A-06918;  NH4.03-1TH1O-002
Putelat, T.; Dawes, J.H.; Willis, J. R.; Aifantis, E. C.
Relaxation oscillations of slip and crack instabilities (solicited)

9:30 - 9:45
EGU2007-A-02314;  NH4.03-1TH1O-003
Balasis, G.; Mandea, M.
CHAMP satellite observations during recent destructive megathrust earthquakes

9:45 - 10:00
EGU2007-A-04829;  NH4.03-1TH1O-004
Eftaxias, K.; Contoyiannis, Y.; Karamanos, K.; Kalimeri, M.; Balasis, G.; Kopanas, J.; Antonopoulos, G.; Nomicos, K. D.
Evidence of a self-affine asperity fault model in preseismic electromagnetic activity


Chairperson: CHELIDZE , T.

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10:30 - 11:00
EGU2007-A-01658;  NH4.03-1TH2O-001
Tsutsui, M.
A method of monitoring earth-crust stress-changes from identifications of source locations of EM pulses excited in the earth (solicited)

11:00 - 11:15
EGU2007-A-04778;  NH4.03-1TH2O-002
Koulouras, G; Kontakos, K; Avgoustis, G; Stonham, J; Ruzhin, Y; Stavrakakis, G; Eftaxias, C; Nomicos, C
Electromagnetic emissions in the 142 to 415 MHZ band

11:15 - 11:30
EGU2007-A-01247;  NH4.03-1TH2O-003
Cavouras, D.; Georgiadis, P.
Application of pattern recognition methods for detecting the existence of EM precursor signals preceding major seismic events

11:30 - 11:45
EGU2007-A-02320;  NH4.03-1TH2O-004
Mandea, M.; Balasis, G.
Occurence of catastrophic geophysical events

11:45 - 12:00
EGU2007-A-04830;  NH4.03-1TH2O-005
Karamanos, K.; Nomikos, C.; Eftaxias, K.
Search for signatures that imply the transition to earthquake nucleation by means of complexity


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