Ambient noise Rayleigh wave tomography across Europe

By Yingjie Yang, M. Ritzwoller, A. Levshin, N. M. Shapiro. 2007

601 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/420fa4d509b7f652e46c2bdb34078b561e922646

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Citations in the corpus

Origin of deep ocean microseisms by using teleseismic body waves (2010, methodology): “…records provided by modern networks provides us with new approaches for seismic tomography [e.g., Shapiro and Campillo, 2004; Shapiro et al., 2005; Sabra et al., 2005; Yang et al., 2007; Stehly et al., 2009] and monitoring [e.g., Sens‐Schönfelder and Wegler, 2006; Brenguier et al., 2008b, 2008a].”
Eikonal tomography: surface wave tomography by phase front tracking across a regional broad‐band seismic array (2009, methodology): “Assuming that the amplitude of the waveform varies smoothly, the eikonal equation states that the gradient of the phase traveltime surface can be used to estimate both the local phase speed and the direction of wave propagation.”
Frequency‐Bessel Transform Method for Effective Imaging of Higher‐Mode Rayleigh Dispersion Curves From Ambient Seismic Noise Data (2019, background): “Ambient seismic noise, which is also called microtremor in the field of geotechnique engineering, is a stochastic wavefield generated by various passive sources (e.g., Okada & Suto, 2003; Yang et al., 2007; Yang & Ritzwoller, 2008).”
Tomography of the Alpine region from observations of seismic ambient noise (2009, background): “, 2007), and to produce large-scale Rayleigh wave group velocity maps across Europe (Yang et al., 2007).”
Determination of surface‐wave phase velocities across USArray from noise and Aki's spectral formulation (2009, methodology): “Distances shorter than two or three wavelengths have typically been avoided in time-domain studies, which depend on the far-field approximation in the interpretation of the Green function [Shapiro et al., 2005; Yao et al., 2006; Yang et al., 2007; Lin et al., 2008].”
Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, methodology): “It was shown to be an efficient tool for seismic tomography [Shapiro et al., 2005; Sabra et al., 2005b; Yao et al., 2006; Yang et al., 2007; Lin et al., 2007; Brenguier et al., 2007].”
Characteristics of ambient seismic noise as a source for surface wave tomography (2008, methodology): “... Korea [Cho et al., 2007], Tibet [Yao et al., 2006], New Zealand [Lin et al., 2007], Iceland [Gudmundsson et al., 2007], and southern Africa (Y. Yang et al., Crustal and uppermost mantle structure in southern Africa revealed from ambient noise and teleseismic tomography, submitted to Geophysical ”
Analysis of ambient noise energy distribution and phase velocity bias in ambient noise tomography, with application to SE Tibet (2009, background): “Sabra et al. 2005; Shapiro et al. 2005; Kang & Shin 2006; Yao et al. 2006, 2008; Lin et al. 2007, 2008; Moschetti et al. 2007; Yang et al. 2007, 2008; Liang & Langston 2008; Zheng et al. 2008) has greatly improved our ability to resolve the shallow crust structure by extracting short periods group”
Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements (2007, methodology): “Obtaining tens of thousands of cross-correlations is common when ambient noise C© 2007 The Authors, GJI, 169, 1239–1260 Journal compilation C© 2007 RAS data processing is performed over large spatial scales such as Europe (e.g. Yang et al. 2007) or North America (e.g. Bensen et al. 2005).”
Retrieval of Moho‐reflected shear wave arrivals from ambient seismic noise (2010, unknown): “E-mail: zwzhan@gmail.com 2Seismological Laboratory, California Institute of Technology, 1200 E. California Blvd, Pasadena, CA 91125, USA Accepted 2010 April 13.”
On establishing the accuracy of noise tomography travel‐time measurements in a realistic medium (2009, background): “One should also note that although group velocity studies (Shapiro et al. 2005; Benson et al. 2007; Cho et al. 2007; Yang et al. 2007) do not initially arrive at the phase travel time, they make group velocity measurements based on this same phase travel time and are therefore affected in the same…”
Broadband ambient noise surface wave tomography across the United States (2008, background): “…settings, such as Southern California [Shapiro et al., 2005; Sabra et al., 2005], the western US [Moschetti et al., 2007; Lin et al., 2008], Europe [Yang et al., 2007], Tibet [Yao et al., 2006], New Zealand [Lin et al., 2007], Korea [Cho et al., 2007], Spain [Villaseñor et al., 2007] and…”