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Moment-tensor inversion of LP events recorded on Etna in 2004 using constraints obtained from wave simulation tests (CROSBI ID 134897)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Lokmer, Ivan ; Bean, Christopher J. ; Saccorotti, Gilberto ; Patane, Domenico Moment-tensor inversion of LP events recorded on Etna in 2004 using constraints obtained from wave simulation tests // Geophysical research letters, 34 (2007), 22; 22316-1-22316-6

Podaci o odgovornosti

Lokmer, Ivan ; Bean, Christopher J. ; Saccorotti, Gilberto ; Patane, Domenico

engleski

Moment-tensor inversion of LP events recorded on Etna in 2004 using constraints obtained from wave simulation tests

The persistent occurrence of long period (LP) events at Mt Etna became apparent with the installation of the first fixed broad-band seismic network in late 2003. Repeating similar LP events from Nov. ‘ 03 to Sept. ‘ 04 indicate a nondestructive source process. We perform moment tensor (MT) inversions on a stacked high S/N ratio representative LP signal, conducting a grid search for the source geometry and L2-inversion for the source time function. Results indicate a NNW-SSE oriented resonating sub-vertical crack as the most probable source. This result is consistent with deformation and GPS observations. Crucial to this result are constraints imposed by detailed 3D full waveform numerical simulations in a heterogeneous tomographic model with topography, and in particular a detailed assessment of the influence of very near surface velocity structure onLPsignals. Pulsating gas injection is hypothesised as the most likely LP trigger.

Etna volcano; moment tensor inversion; LP activity

nije evidentirano

nije evidentirano

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nije evidentirano

Podaci o izdanju

34 (22)

2007.

22316-1-22316-6

objavljeno

0094-8276

Povezanost rada

Geologija

Indeksiranost