Introduction to the special issue of the Consortium of Organizations for Strong Motion Observation Systems (COSMOS) international guidelines for applying noninvasive geophysical techniques to characterize seismic site conditions

Yong, Alan; Askan, Ayşegül; Cassidy, John F.; D’Amico, Sebastiano; Parolai, Stefano; Pilz, Marco; Stephenson, William J.

doi:10.1007/s10950-022-10104-w

Cited by 4 publications

(1 citation statement)

References 41 publications

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“…Surface waves are recorded based on the property of geometrical dispersion which makes the velocity of propagating Rayleigh waves as frequency dependent in vertically heterogeneous sedimentary media. The experimental dispersion curve can be extracted from the generated microtremor array data using a variety of processing techniques (Foti et al, 2018; Yong et al, 2022 and references therein) and is used further for inversion, aiming to get the 1D V S profile beneath the array site. The most popular techniques among various array signal analysis tools are frequency–wavenumber (F-K) and spatially autocorrelation (SPAC) (Hayashi et al, 2022).…”

Section: Methodology and Data Analysismentioning

confidence: 99%

Site response analysis beneath the Kashmir basin (NW Himalaya) using ambient noise

Gupta,

Parvez,

Khan

2023

Earthquake Spectra

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Deep sedimentary valleys entrap and amplify seismic waves, which is further responsible for site-specific amplification over the allied region. Kashmir valley is a deep and active sedimentary basin in the northwest portion of the Himalayan lap. To characterize the site response for the intermountain Kashmir valley for the first time, we acquire single station microtremor measurements using Lennartz (three components/5s seismometer) at 141 sites with a grid of (5 km × 5 km) and two-dimensional (2D) array measurements using seven units of recording station of different geometry pattern at 38 sites across different lithological setup within the basin. We present here (1) a first-order predominant fundamental frequency (0.21–10.19 Hz) and subsequent sedimentary thickness maps for the entire valley, reflecting deep deposition with spatial heterogeneity in the area using the horizontal-to-vertical spectral ratio (HVSR) technique; (2) spatial classification of generated HVSR curves linking subsurface geomorphology and post strong ground-motion scenario in the valley; (3) extraction of the best dispersion characteristics of Rayleigh waves (fundamental mode) from all recorded vertical signals at each array site using frequency–wavenumber (F-K) method with an emphasis on signal synchronicity; and (4) retrieval of one-dimensional (1D) shear wave velocity ( VS) profiles across the valley from the inversion of dispersion curves using the neighborhood algorithm. Distinct model parameterizations were tested for the inversion to achieve the optimal inversion misfit. The collocated 1D VS profiles are consistent with newly drilled borehole logs information. Besides, the presented first-ever ambient noise survey–based site response study meets the objectives of site-specific seismic hazard and risk analysis of the Kashmir valley at the regional scale.

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Section: Methodology and Data Analysismentioning

confidence: 99%

Site response analysis beneath the Kashmir basin (NW Himalaya) using ambient noise

Gupta,

Parvez,

Khan

2023

Earthquake Spectra

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Estimating S-wave velocity profiles from horizontal-to-vertical spectral ratios based on deep learning

Hayashi,

Suzuki,

Inazaki

et al. 2024

Soils and Foundations

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Subsurface structure identification at the blind prediction site of ESG6 based on the earthquake-to-microtremor ratio method and diffuse field concept for earthquakes

Nagashima

Kawase

Nakano³

et al. 2023

Earth Planets Space

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We participated in the blind prediction exercise organized by the committee of the blind prediction experiment during the 6th International Symposium on Effects of Surface Geology on Seismic Motion (CBP-ESG6). In response to the committee's request, we identified the ground velocity structure from microtremors observed at a target site as the first step of the exercise. First, we calculated the horizontal-to-vertical spectral ratio of microtremors (MHVR) at the target site from the distributed microtremor data collected in the vicinity of the target site in Kumamoto Prefecture. Then, we converted the MHVR into a pseudo horizontal-to-vertical spectral ratio of earthquake (pEHVR) using the previously proposed and validated earthquake-to-microtremor ratio (EMR) method, where an empirically obtained EMR is used to convert MHVR into pEHVR. Next, we inverted the S-wave and P-wave velocity structures based on the pEHVR and the diffuse field concept for earthquakes. The theoretical EHVR calculated from the identified velocity structure reproduced the pEHVR quite well in the frequency range of 0.1–22 Hz. After the collection of the blind prediction results by all the participants, the CBP-ESG6 released the observed earthquake records, a preferred model based on the P–S logging data from the in-situ borehole measurement combined with the generic deeper structure, and the average of all the predicted structures by the participants. Notably, our inverted structure was found to be close to the preferred model and the averaged one of all the blind prediction participants, despite some minor differences in the horizontal site amplification factor around the maximum peak frequency at 0.8–1 Hz. Graphical Abstract

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Introduction to the special issue of the Consortium of Organizations for Strong Motion Observation Systems (COSMOS) international guidelines for applying noninvasive geophysical techniques to characterize seismic site conditions

Cited by 4 publications

References 41 publications

Site response analysis beneath the Kashmir basin (NW Himalaya) using ambient noise

Site response analysis beneath the Kashmir basin (NW Himalaya) using ambient noise

Estimating S-wave velocity profiles from horizontal-to-vertical spectral ratios based on deep learning

Subsurface structure identification at the blind prediction site of ESG6 based on the earthquake-to-microtremor ratio method and diffuse field concept for earthquakes

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