Finding sets of acceptable solutions with a genetic algorithm with application to surface wave group dispersion in Europe
We discuss the use of a genetic algorithm (GA) to invert data for many acceptable solutions,
in contrast to inversion for a single,“optimum” solution. The GA is a directed search method …
in contrast to inversion for a single,“optimum” solution. The GA is a directed search method …
The contrast in upper mantle shear-wave velocity between the East European Platform and tectonic Europe obtained with genetic algorithm inversion of Rayleigh …
Summary The stable, Precambrian East European Platform adjoins the younger, tectonically
active regions of central and western Europe along a distinct crustal boundary, the Tornquist …
active regions of central and western Europe along a distinct crustal boundary, the Tornquist …
Improved Monte Carlo inversion of surface wave data
LV Socco, D Boiero - Geophysical Prospecting, 2008 - earthdoc.org
Inversion of surface wave data suffers from solution non‐uniqueness and is hence strongly
biased by the initial model. The Monte Carlo approach can handle this non‐uniqueness by …
biased by the initial model. The Monte Carlo approach can handle this non‐uniqueness by …
Monte-Carlo inversion for a global shear-velocity model of the crust and upper mantle
NM Shapiro, MH Ritzwoller - Geophysical Journal International, 2002 - academic.oup.com
We describe a method to invert surface wave dispersion data for a model of shear velocities
with uncertainties in the crust and uppermost mantle. The inversion is a multistep process …
with uncertainties in the crust and uppermost mantle. The inversion is a multistep process …
Constraints on the S wave velocity structure in a continental shield from surface wave data: Comparing linearized least squares inversion and the direct search …
JA Snoke, M Sambridge - Journal of Geophysical Research …, 2002 - Wiley Online Library
In their study of upper mantle structure beneath the Paraná Basin of SE Brazil, Snoke and
James [1997] concluded, on the basis of a linearized least squares inversion (LLSI) of …
James [1997] concluded, on the basis of a linearized least squares inversion (LLSI) of …
Exploring the model space and ranking a best class of models in surface-wave dispersion inversion: Application at European strong-motion sites
The inversion of surface-wave dispersion curve to derive shear-wave velocity profile is a
very delicate process dealing with a nonunique problem, which is strongly dependent on the …
very delicate process dealing with a nonunique problem, which is strongly dependent on the …
Application of simulated annealing inversion on high-frequency fundamental-mode Rayleigh wave dispersion curves
D Pei, JN Louie, SK Pullammanappallil - Geophysics, 2007 - library.seg.org
The simulated annealing (SA) inversion technique has been successfully applied for solving
various nonlinear geophysical problems. Following previous developments, we modified the …
various nonlinear geophysical problems. Following previous developments, we modified the …
An upper-mantle S-wave velocity model for Northern Europe from Love and Rayleigh group velocities
A model of upper-mantle S-wave velocity and transverse anisotropy beneath northwestern
Europe is presented, based on regional surface wave observations. Group velocities for …
Europe is presented, based on regional surface wave observations. Group velocities for …
Genetic Algorithms Inversion of Lithospheric Structure From Surface Wave Dispersion.
Y Shi, W Jin - Chinese Science Abstracts Series B, 1995 - infona.pl
The authors apply genetic algorithms to seismic surface wave inversion to deduce
lithospheric structure from dispersion data. Synthetic data are used to test the algorithms. It is …
lithospheric structure from dispersion data. Synthetic data are used to test the algorithms. It is …
Joint inversion of surface wave dispersion and receiver functions: a Bayesian Monte-Carlo approach
W Shen, MH Ritzwoller… - Geophysical Journal …, 2013 - academic.oup.com
A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …