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Nonlinear inversion of tilt‐affected very long period records of explosive eruptions at Fuego volcano
Author(s) -
Waite Gregory P.,
Lanza Federica
Publication year - 2016
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.983
H-Index - 232
eISSN - 2169-9356
pISSN - 2169-9313
DOI - 10.1002/2016jb013287
Subject(s) - geology , waveform , seismology , volcano , geodesy , inversion (geology) , explosive material , seismogram , tectonics , physics , chemistry , organic chemistry , quantum mechanics , voltage
Magmatic processes produce a rich variety of volcano seismic signals, ranging over several orders of magnitude in frequency and over a wide range of mechanism types. We examined signals from 400 to 10 s period associated with explosive eruptions at Fuego volcano, Guatemala, that were recorded over 19 days in 2009 on broadband stations with 30 s and 60 s corner periods. The raw data from the closest stations include tilt effects on the horizontal components but also have significant signal at periods below the instrument corners on the vertical components, where tilt effects should be negligible. We address the problems of tilt‐affected horizontal waveforms through a joint waveform inversion of translation and rotation, which allows for an investigation of the varying influence of tilt with period. Using a phase‐weighted stack of six similar events, we invert for source moment tensor using multiple bands. We use a grid search for source type and constrained inversions, which provides a quantitative measure of source mechanism reliability. The 30‐10 s band‐pass results are consistent with previous work that modeled data with a combined two crack or crack and pipe model. At the longest‐period band examined, 400‐60 s, the source mechanism is like a pipe that could represent the shallowest portion of the conduit. On the other hand, source mechanisms in some bands are unconstrained, presumably due to the combined tilt‐dominated and translation‐dominated signals, which are not coincident in space and have different time spans.

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