Observatoire de la Côte d'Azur (OCA)
Université Côte D'Azur (UniCA)
France
Plane shallow dipping to the East (strike 179) shown.
Rupt very concentrated around the hypocenter, far from and much deeper than the trench.
Thanks to seismic records through IRIS
Plane shallow dipping to the East (strike 179) shown.
Rupt very concentrated around the hypocenter, far from and much deeper than the trench.
Thanks to seismic records through IRIS
Plane oriented NW-SE (dipping to the NE) shown.
Rupt propagation mainly to the NW, surface rupture likely.
Thanks to seismic records through IRIS
Plane oriented NW-SE (dipping to the NE) shown.
Rupt propagation mainly to the NW, surface rupture likely.
Thanks to seismic records through IRIS
Thanks to the seismic records provided through IRIS
Thanks to the seismic records provided through IRIS
Rupture plane not selected in an automated way. The two planes are shown.
The focal mechanism used is from GFZ
Rupture plane not selected in an automated way. The two planes are shown.
The focal mechanism used is from GFZ
Rupture plane not selected in an automated way. The two planes are shown.
Rupture plane not selected in an automated way. The two planes are shown.
Plane striking N343 (NNW-SSE) shown.
Rupture direction to the South-East constrained by nearby stations (quite opposite to the USGS result).
Thanks to seismic records through IRIS
Plane striking N343 (NNW-SSE) shown.
Rupture direction to the South-East constrained by nearby stations (quite opposite to the USGS result).
Thanks to seismic records through IRIS
Preferred rupture plane (strike,dip,rake) : 50 20 112
with confidence : 47.%
Discrimination among the two nodal planes
may be considered reliable only if
this confidence is larger or equal to 70%
Preferred rupture plane (strike,dip,rake) : 50 20 112
with confidence : 47.%
Discrimination among the two nodal planes
may be considered reliable only if
this confidence is larger or equal to 70%
Rupture plane not selected in an automated way. Plane dip to the NE (strike 326) shown.
Rupture propagation mainly to the SE.
Thanks to seismic records through IRIS
Rupture plane not selected in an automated way. Plane dip to the NE (strike 326) shown.
Rupture propagation mainly to the SE.
Thanks to seismic records through IRIS
EW nodal plane preferred with confidence 65% as the rupture plane. Rupt propagation mainly to the East.
Thanks to seismic records from KOERI
EW nodal plane preferred with confidence 65% as the rupture plane. Rupt propagation mainly to the East.
Thanks to seismic records from KOERI
Thanks to the seismic records provided through IRIS and SCEDC
Thanks to the seismic records provided through IRIS and SCEDC
sismoazur.oca.eu#/focal_mecha...
emsc-csem.org/Earthquake_d...
Thanks to the seismic records from Spain and Portugal provided through IGN and IRIS
sismoazur.oca.eu#/focal_mecha...
emsc-csem.org/Earthquake_d...
Thanks to the seismic records from Spain and Portugal provided through IGN and IRIS
Mw 4.4
Joint inversion of waveforms and first motions.
Thanks to the seismic records provided from Portugal through IRIS
Mw 4.4
Joint inversion of waveforms and first motions.
Thanks to the seismic records provided from Portugal through IRIS