A Breviary of Seismic Tomography: Body wave amplitudes: observation and interpretation

By Guust Nolet. 2008

168 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/bb8094e32255b591f66f5da198bcdee749f6c0db

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Citations in the corpus

AxiSEM: broadband 3-D seismic wavefields in axisymmetric media (2014, background): “Most modern measurements of “traveltimes”, such as cross-correlation (Nolet, 2008), time–frequency phase delays (Fichtner et al., 2008), or instantaneous phase (Bozdag et al., 2011) are based on waveforms, and therefore necessitate full wavefield modeling.”
Full Waveform Inversion and the Truncated Newton Method (2013, methodology): “While standard seismic methods rely on the extraction of particular observables from the seismic data, such as travel-times for tomography strategies [56], full waveform inversion (FWI) is a particular seismic method which aims to interpret the whole seismic data, accounting for all seismic events (”
A simple method for determining the spatial resolution of a general inverse problem (2012, methodology): “(15) If the summation ci is equal to 1, the solution parameter mi can be considered as unbiased under the condition that eqs (13) or (14) yield a true average (Nolet 2008).”
Transdimensional tomography with unknown data noise (2012, background): “Due to the increasing quantity and quality of seismic data, the number of overlapping tomographic models and their consistency has dramatically increased in recent years (Nolet 2008).”
On the use of sensitivity tests in seismic tomography (2016, unknown): “(10): where R = G − g G is the more commonly used resolution matrix (e.g. Nolet 2008).”
Hessian kernels of seismic data functionals based upon adjoint techniques (2011, background): “…GJI, 185, 775–798 Geophysical Journal International C© 2011 RAS traveltimes (see Section 4), to study wave propagation through complex media (e.g. Baig & Dahlen 2004), or to design locally independent model parameters as it is classically done in Partitioned Waveform Inversion (Nolet 1990, 2008).”