- ISSN: 0812-3985
- E-ISSN: 1834-7533
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oa Development and numerical tests of a Bayesian approach to inferring shallow velocity structures using microtremor arrays
- Australian Society of Exploration Geophysicists
- Source: Exploration Geophysics, Volume 49, Issue 6, Nov 2018, p. 881 - 890
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- 17 Jan 2018
- 19 Jan 2018
- 01 Nov 2018
Abstract
We propose an empirical Bayesian approach to inferring shallow (depth ranges from a few to several tens of metres) S-wave velocity structures using microtremor arrays and execute numerical tests to assess the feasibility of this approach. In our approach, the estimate of the S-wave structure (posterior) is derived from an empirical S-wave structure model (prior) and phase velocities of Rayleigh waves obtained with microtremor arrays. In other words, we aim to find a model that is close to the empirical model and is able to explain phase velocities with a 1D surface-wave theory. The inversion is stabilised by the constraints from the prior model so that model parameterisation with many thin layers can be adopted. The velocity structure is individually estimated for each of two cases (assumptions): the case where we assume fundamental-mode dominance and the case where we take into account the higher modes. Optimal values of the model parameters (e.g. a thickness parameter) are found, based on Akaike’s Bayesian Information Criterion (ABIC), and the choice of the better assumption of the surface-wave theory is also based on ABIC. Numerical tests, where synthetic data is generated from a horizontally stratified two-layer model, indicate that the relative weight between a prior model and the observed data is appropriately adjusted by ABIC. It is revealed that a value of the thickness parameter required to reproduce the given two-layer model is successfully found by ABIC. We also suggest that we can make a plausible choice of the assumption of the surface-wave theory with ABIC, unless observation error is extremely large.
,We have developed an empirical Bayesian approach to inferring shallow S-wave velocity structures. This approach has the potential to automatically determine the number of layers of a velocity structure model as well as to confirm the plausible assumption of a surface-wave theory.
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