Performance of a Rotational Sensor to Decipher Volcano Seismic Signals on Etna, Italy

نویسندگان

چکیده

Abstract Volcano‐seismic signals such as long‐period events and tremor are important indicators for volcanic activity unrest. However, their wavefield is complex characterization location using traditional seismological instrumentation often difficult. In 2019 we recorded the full seismic a newly developed 3C rotational sensor co‐located with seismometer on Etna, Italy. We compare performance of sensor, Istituto Nazionale di Geofisica e Vulcanologia‐Osservatorio Etneo (INGV‐OE) network respect to analysis volcano‐seismic signals. create event catalogs volcano‐tectonic (VT) (LP) combining STA/LTA algorithm cross‐correlations. The detection based reliable seismometer‐based detection. LP dominated by SH‐type waves. Derived SH phase velocities range from 500 1,000 m/s 300–400 tremor. SH‐waves compose during weak SH‐ SV‐waves sustained strombolian activity. derive back azimuths (a) horizontal components (b) vertical rotation rate transverse acceleration. estimated consistent INGV‐OE VT an epicentral distance larger than 3 km some closer events, in main crater area. Measuring can reliably analyze azimuths, composition VT, regions that difficult access volcanoes.

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ژورنال

عنوان ژورنال: Journal Of Geophysical Research: Solid Earth

سال: 2022

ISSN: ['2169-9356', '2169-9313']

DOI: https://doi.org/10.1029/2021jb023617