Tomography of the Alpine region from observations of seismic ambient noise

By Laurent Stehly, B. Fry, Michel Campillo, N. M. Shapiro, J. Guilbert, Lapo Boschi, Domenico Giardini. 2009

186 citations recorded by the source corpus.

Subfields: Geophysics, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/9b57d9221a140a6dcd781d947b2026752d0bc5d8

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In Geophysics

In Ocean Engineering

Citations in the corpus

Structure of young East Pacific Rise lithosphere from ambient noise correlation analysis of fundamental- and higher-mode Scholte-Rayleigh waves (2011, methodology): “Ambient noise or coda-wave cross-correlation has been used to estimate surface-wave propagation (Green’s functions) between receivers (Campillo and Paul, 2003; Shapiro and Campillo, 2004), and therefore has been widely used for surface-wave tomography to investigate crustal structure all over the wo”
Origin of deep ocean microseisms by using teleseismic body waves (2010, methodology): “Application of this principle to large amount of continuous digital seismic 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”
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.”
Transdimensional tomography with unknown data noise (2012, background): “…last decade, transdimensional inversion has become popular in Earth sciences and has been applied to a wide range of areas (e.g. Malinverno 2002; Stephenson et al. 2004, 2006; Jasra et al. 2006; Hopcroft et al. 2009; Charvin et al. 2009; Gallagher et al. 2011; Dettmer et al. 2010; Luo 2010;…”
Transdimensional inversion of receiver functions and surface wave dispersion (2012, methodology): “…RFs jointly with observations based on the cross-correlation of ambient noise recorded at nearby receivers [Campillo and Paul, 2003; Shapiro and Campillo, 2004; Stehly et al., 2009], which 3 of 24 provides apparent travel times of surface waves at periods 1–30 s (mostly sensitive to the crust).”