دورية أكاديمية

One-Year Seismic Survey of the Tectonic CO 2 -Rich Site of Mefite d'Ansanto (Southern Italy): Preliminary Insights in the Seismic Noise Wavefield.

التفاصيل البيبلوغرافية
العنوان: One-Year Seismic Survey of the Tectonic CO 2 -Rich Site of Mefite d'Ansanto (Southern Italy): Preliminary Insights in the Seismic Noise Wavefield.
المؤلفون: Morabito, Simona, Cusano, Paola, Galluzzo, Danilo, Gaudiosi, Guido, Nardone, Lucia, Del Gaudio, Pierdomenico, Gervasi, Anna, La Rocca, Mario, Milano, Girolamo, Petrosino, Simona, Zuccarello, Luciano, Manzo, Roberto, Buonocunto, Ciro, Di Luccio, Francesca
المصدر: Sensors (14248220); Feb2023, Vol. 23 Issue 3, p1630, 18p
مصطلحات موضوعية: SEISMIC surveys, EARTHQUAKE zones, MICROSEISMS, SEISMIC arrays, CARBON dioxide, RAYLEIGH waves
مصطلحات جغرافية: ITALY
مستخلص: A passive seismic experiment is carried out at the non-volcanic highly degassing site of Mefite d'Ansanto located at the northern tip of the Irpinia region (southern Italy), where the 1980 MS 6.9 destructive earthquake occurred. Between 2020 and 2021, background seismic noise was recorded by deploying a broadband seismic station and a seismic array composed of seven 1 Hz three-component sensors. Using two different array configurations, we were allowed to explore in detail the 1–20 Hz frequency band of the seismic noise wavefield as well as Rayleigh wave phase velocities in the 400–800 m/s range. Spectral analyses and array techniques were applied to one year of data showing that the frequency content of the signal is very stable in time. High frequency peaks are likely linked to the emission source, whereas at low frequencies seismic noise is clearly correlated to meteorological parameters. The results of this study show that small aperture seismic arrays probe the subsurface of tectonic CO2-rich emission areas and contribute to the understanding of the link between fluid circulation and seismogenesis in seismically active regions. [ABSTRACT FROM AUTHOR]
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قاعدة البيانات: Complementary Index
الوصف
تدمد:14248220
DOI:10.3390/s23031630