Determination of the influence zone for surface wave paths

By K. Yoshizawa, Brian L. N. Kennett. 2002

148 citations recorded by the source corpus.

Subfields: Geophysics, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/4a21dc40365baac162e95efa4841e8762f86ff33

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In Ocean Engineering

Citations in the corpus

Three‐dimensional sensitivity kernels for surface wave observables (2004, background): “... waves (Yomogida 1992; Marquering et al. 1998; Friederich 1999; Marquering et al. 1999; Dahlen et al. 2000; Hung et al. 2000; Dalkolmo & Friederich 2000; Zhao et al. 2000; K´ arason & van der Hilst 2001; Montelli et al. 2003); surface waves (Snieder 1986; Snieder & Nolet 1987; Yomogida & Aki 1987”
Regional tomographic inversion of the amplitude and phase of Rayleigh waves with 2-D sensitivity kernels (2006, background): “In recent years, the finite-frequency properties of surface waves have been considered in a number of global surface wave tomography studies (Clevede et al. 2000; Spetzler et al. 2002; Ritzwoller et al. 2002; Yoshizawa & Kennett 2002; Zhou et al. 2004).”
Eikonal tomography: surface wave tomography by phase front tracking across a regional broad‐band seismic array (2009, methodology): “…speeds in the medium of propagation using ray theory with straight or potentially bent rays (e.g. Trampert & Woodhouse 1996; Ekstrom et al. 1997; Ritzwoller & Levshin 1998; Yoshizawa & Kennett 2002) or finite frequency kernels (e.g. Dahlen et al. 2000; Ritzwoller et al. 2002; Levshin et al. 2005).”
An anisotropic shear velocity model of the Earth's mantle using normal modes, body waves, surface waves and long-period waveforms (2014, methodology): “Some methods to specifically isolate and constrain overtone dispersion have been developed (e.g. van Heijst & Woodhouse 1997; Yoshizawa & Kennett 2002a; Visser & Trampert 2008).”
Broadband ambient noise surface wave tomography across the United States (2008, background): “In recent years, surface wave studies have increasingly moved toward diffraction tomography using spatially extended finite-frequency sensitivity kernels based on the Born/Rytov approximation [e.g., Spetzler et al., 2002; Ritzwoller et al., 2002; Yoshizawa and Kennett, 2002].”
Ambient noise Rayleigh wave tomography of New Zealand (2007, methodology): “In recent years, surface wave studies have increasingly used diffraction tomography based on spatially extended finite-frequency sensitivity kernels derived from the Born/Rytov approximation (e.g. Spetzler et al. 2002; Ritzwoller et al. 2002; Yoshizawa & Kennett 2002; Zhou et al. 2004; many others).”
Surface-wave array tomography in SE Tibet from ambient seismic noise and two-station analysis: I - Phase velocity maps (2006, unknown): “Other reasons for the frequency-dependent discrepancy of phase velocities between the two methods include the fact that the surfacewave sensitivity zone in the TS method is much larger than the zone of sensitivity to structure in the case of the EGF analysis as shown in Fig. 12(d), especially at lon”
Global P and PP traveltime tomography: rays versus waves (2004, background): “…two and three dimensions (Gelchinsky 1985; Woodward 1992; Yomogida 1992; Cardimora & Garmany 1993; Stark & Nikolayev 1993; Vasco & Majer 1993; Li & Tanimoto 1993; Marquering et al. 1998, 1999; Dahlen et al. 2000; Hung et al. 2000; Zhao et al. 2000; Ritzwoller et al. 2002; Yoshizawa & Kennett 2002).”
Global surface wave diffraction tomography (2002, methodology): “[Yoshizawa and Kennett, 2002] argue that the primary ‘‘zone of influence’’ spans only about one-third of the width of the first Fresnel zone, so N = 18 is the value that should be used in surface wave tomography.”
Ambient noise Rayleigh wave tomography across Europe (2007, methodology): “…wave studies have increasing moved toward diffraction tomography using spatially extended finite-frequency sensitivity kernels based on the Born/Rytov approximation (e.g. Clevede et al. 2000; Spetzler et al. 2002; Ritzwoller et al. 2002; Yoshizawa & Kennett 2002; Zhou et al. 2004, many others).”