Relevant bibliographies by topics / Rayleigh-to-love wave ratio

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Academic literature on the topic 'Rayleigh-to-love wave ratio'

Author: Grafiati
Published: 4 June 2021
Last updated: 7 February 2022

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Journal articles on the topic "Rayleigh-to-love wave ratio"

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Li, Jing, Sherif Hanafy, Zhaolun Liu, and Gerard T. Schuster. "Wave-equation dispersion inversion of Love waves." GEOPHYSICS 84, no. 5 (2019): R693—R705. http://dx.doi.org/10.1190/geo2018-0039.1.

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We present a theory for wave-equation inversion of Love-wave dispersion curves, in which the misfit function is the sum of the squared differences between the wavenumbers along the predicted and observed dispersion curves. Similar to inversion of Rayleigh-wave dispersion curves, the complicated Love-wave arrivals in traces are skeletonized as simpler data, namely, the picked dispersion curves in the [Formula: see text] domain. Numerical solutions to the SH-wave equation and an iterative optimization method are then used to invert these dispersion curves for the S-wave velocity model. This proc
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TOKIMATSU, Kohji, and Hiroshi ARAI. "EFFECTS OF RAYLEIGH TO LOVE WAVE AMPLITUDE RATIO ON MICROTREMOR HORIZONTAL-TO-VERTICAL SPECTRAL RATIO." Journal of Structural and Construction Engineering (Transactions of AIJ) 63, no. 511 (1998): 69–75. http://dx.doi.org/10.3130/aijs.63.69_5.

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Malkoti, Ajay, Arjun Datta, and Shravan M. Hanasoge. "Rayleigh-wave H/V ratio measurement from ambient noise cross-correlations and its sensitivity to VP: a numerical study." Geophysical Journal International 227, no. 1 (2021): 472–82. http://dx.doi.org/10.1093/gji/ggab228.

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SUMMARY The promise of passive seismology has increasingly been realized in recent years. Given the expense in installing and maintaining seismic station networks, it is important to extract as much information from the measurements as possible. In this context, the ellipticity or H/V amplitude ratio of Rayleigh waves can prove to be a valuable observable in ambient noise seismology due to its complimentary sensitivity to subsurface structure, compared to phase and group-velocity dispersion, as well as its potential for constraining VP structure in addition to VS. However, the suitability of t
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Hawkins, Rhys, and Malcolm Sambridge. "An Adjoint Technique for Estimation of Interstation Phase and Group Dispersion from Ambient Noise Cross Correlations." Bulletin of the Seismological Society of America 109, no. 5 (2019): 1716–28. http://dx.doi.org/10.1785/0120190060.

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Abstract A method of extracting group and phase velocity dispersions jointly for Love‐ and Rayleigh‐wave observations is presented. This method uses a spectral element representation of a path average Earth model parameterized with density, shear‐wave velocity, radial anisotropy, and VP/VS ratio. An initial dispersion curve is automatically estimated using a heuristic approach to prevent misidentification of the phase. A second step then more accurately fits the observed noise correlation function (NCF) between interstation pairs in the frequency domain. For good quality cross correlations wit
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Mendecki, Maciej J., Barbara Bieta, Mateusz Mateuszów, and Paweł Suszka. "Comparison of site effect values obtained by HVSR and HVSRN methods for single-station measurements in Tarnówek, South-Western Poland." Contemporary Trends in Geoscience 5, no. 1 (2016): 18–27. http://dx.doi.org/10.1515/ctg-2016-0002.

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Abstract This study compares the HVSR technique (Horizontal to Vertical Spectral Ratio), based on seismic event records, and the HVSRN technique (Horizontal to Vertical Spectral Ratio of Noise) using seismic noise registrations. Both methods allow us to study the amplification phenomenon of a horizontal component of seismic waves when the waves reach loose sediments in subsurface layers. The seismic data were measured at a three-component single seismic station located in the village of Tarnówek, in the Legnica-Głogów Copper District. The results of the study demonstrate that average HVSRN and
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Tanimoto, Toshiro, Céline Hadziioannou, Heiner Igel, Joachim Wasserman, Ulrich Schreiber, and André Gebauer. "Estimate of Rayleigh-to-Love wave ratio in the secondary microseism by colocated ring laser and seismograph." Geophysical Research Letters 42, no. 8 (2015): 2650–55. http://dx.doi.org/10.1002/2015gl063637.

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Tanimoto, Toshiro, Céline Hadziioannou, Heiner Igel, et al. "Seasonal variations in the Rayleigh-to-Love wave ratio in the secondary microseism from colocated ring laser and seismograph." Journal of Geophysical Research: Solid Earth 121, no. 4 (2016): 2447–59. http://dx.doi.org/10.1002/2016jb012885.

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Yuan, Siyuan, Ariel Lellouch, Robert G. Clapp, and Biondo Biondi. "Near-surface characterization using a roadside distributed acoustic sensing array." Leading Edge 39, no. 9 (2020): 646–53. http://dx.doi.org/10.1190/tle39090646.1.

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Due to the broadband nature of distributed acoustic sensing (DAS) measurement, a roadside section of the Stanford DAS-2 array can record seismic signals from various sources. For example, it measures the earth's quasistatic deformation caused by the weight of cars (less than 0.8 Hz) as well as Rayleigh waves induced by earthquakes (less than 3 Hz) and by dynamic car-road interactions (3–20 Hz). We directly utilize the excited surface waves for shallow shear-wave velocity inversion. Rayleigh waves induced by passing cars have a consistent fundamental mode and a noisier first mode. By stacking d
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Tanimoto, Toshiro, Chin-Jen Lin, Céline Hadziioannou, Heiner Igel, and Frank Vernon. "Estimate of Rayleigh-to-Love wave ratio in the secondary microseism by a small array at Piñon Flat observatory, California." Geophysical Research Letters 43, no. 21 (2016): 11,173–11,181. http://dx.doi.org/10.1002/2016gl071133.

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Tsuno, Seiji, Andi Muhamad Pramatadie, Yadab P. Dhakal, Kosuke Chimoto, Wakana Tsutsumi, and Hiroaki Yamanaka. "Long-Period Ground Motions Observed in the Northern Part of Kanto Basin, During the 2011 off the Pacific Coast of Tohoku Earthquake, Japan." Journal of Disaster Research 8, sp (2013): 781–91. http://dx.doi.org/10.20965/jdr.2013.p0781.

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During the 2011 off the Pacific coast of Tohoku earthquake (Mw 9.0), strong ground motions were observed at many seismic stations in the Tokyo Metropolitan Area located about 200 km away from the southern edge of the earthquake source fault. Large earthquake responses in high-rise buildings having long natural periods of several seconds were also observed. The largest ground responses for a period of 4 to 5 seconds were observed locally in Oyama (K-NET TCG012) and Koga (K-NET IBR009) on the border between Tochigi and Ibaraki Prefectures in the northern part of Kanto basin. Geophysical informat
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Dissertations / Theses on the topic "Rayleigh-to-love wave ratio"

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Sethi, Shipra. "Secondary microseisme Love wave generation." Thesis, Université de Paris (2019-....), 2019. https://theses.md.univ-paris-diderot.fr/SETHI_Shipra_va2.pdf.

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Le bruit sismique est l'oscillation continue de la Terre enregistrée à chaque station en l'absence de tremblement de terre. Il résulte de l'interaction entre l'atmosphère, les océans et la terre solide. Le signal dominant, appelé microséismes secondaires dans la bande de fréquences 0,1-0,3 Hz, a pour origine l'interaction non linéaire entre des ondes de gravité océaniques de même fréquence et de directions opposées. Les fluctuations de pression qui en résultent près de la surface de l'océan génèrent un signal sismique. Le signal dominant est constitué d'ondes de Rayleigh (R). Plusieurs études
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Conference papers on the topic "Rayleigh-to-love wave ratio"

1

Zhao, Yumin, Yunyue Elita Li, and Bei Li. "Estimation of Rayleigh to Love waves ratio from ambient noise recorded by DAS." In First International Meeting for Applied Geoscience & Energy. Society of Exploration Geophysicists, 2021. http://dx.doi.org/10.1190/segam2021-3585407.1.

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