This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: http://doi.org/10.1785/0220210349. This is version 1 of this Preprint.
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Abstract
Distributed acoustic sensing is an ideal tool for ambient noise tomography owing to the dense spatial measurements and the ability to continuously record in harsh environments, such as underwater. We demonstrate the ability to image a complex underwater basin using ambient noise recorded on a fiber deployed offshore Greece. A two-dimensional shear-wave velocity model was derived by analyzing Scholte-wave dispersion. In addition, extremely detailed frequency-dependent resonance and wave propagation characteristics were revealed by computing power spectral densities (PSD) and auto-correlations (AC), respectively. These observations provide crucial information on lateral and vertical wave propagation, and were used to further constrain the velocity model. The analysis reveals significant lateral variations across the short 2.5 km long fiber segment, including basin edge effects and scattered waves. Waveform simulations further support the obtained model. Our results demonstrate the advantages of incorporating PSD and AC observations into ambient noise-based imaging.
DOI
https://doi.org/10.31223/X5XK8P
Subjects
Earth Sciences, Geophysics and Seismology
Keywords
Ambient noise tomography, Distributed acoustic sensing, Seismic resonance, Scholte waves, Subsurface imaging
Dates
Published: 2021-09-22 10:02
License
CC BY Attribution 4.0 International
Additional Metadata
Data Availability (Reason not available):
Simulated and observed DAS earthquakes are available on https://osf.io/98cnk/ and https://osf.io/4bjph/, respectively.
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