Inferring upper-mantle temperatures from seismic velocities

By F. Cammarano, S. Goes, Pierre Vacher, Domenico Giardini. 2003

543 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/0bb00f2838773100306d5780f27e035c4066dc1c

How researchers see this paper

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

In Geophysics

Citations in the corpus

Integrated geophysical‐petrological modeling of the lithosphere and sublithospheric upper mantle: Methodology and applications (2008, background): “The latter, on the 11 of 36 other hand, is of primary importance due to its sensitivity to temperature and melt anomalies [Sobolev et al., 1996;Goes et al., 2000;Cammarano et al., 2003].”
Models of large‐scale viscous flow in the Earth's mantle with constraints from mineral physics and surface observations (2006, methodology): “A more detailed treatment of the shallowest mantle would need to consider the non-linear dependence of seismic velocity on temperature anomalies; the same temperature variation causes larger s wave speed variation at lower temperature than at higher temperature (Cammarano et al. 2003).”
Geodesy constraints on the interior structure and composition of Mars (2011, background): “1.4 −0.010 Table B.12: Thermoelastic constants at STP conditions (P = 105Pa, T = 298K) (Verhoeven et al., 2005; Cammarano et al., 2003) for the mantle. ρ, KS , and µ are the density, the bulk modulus, and the shear modulus.”
Thermodynamics of mantle minerals - II. Phase equilibria (2011, methodology): “Several so-called hybrid models have appeared, in which a model of physical properties is combined with a description of phase equilibria from another source (Ita & Stixrude 1992; Cammarano et al. 2003; Hacker et al. 2003).”
Temperature, lithosphere‐asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities (2015, methodology): “…using a nonlinear inversion and laboratory measurements of the density and elastic moduli of various mantle minerals at high temperatures and pressures [e.g., Goes et al., 2000; Röhm et al., 2000; Goes and Van der Lee, 2002; Cammarano et al., 2003; Shapiro and Ritzwoller, 2004a; AN ET AL.”
Joint inversion of seismic and gravity data for lunar composition and thermal state (2007, background): “As most of the material (>80 per cent, Canup 2004) making up the Moon is derived from the mantle of the impactor any present-day Earth–Moon differences are most easily explained, at least to first order, as originating from the distinct chemical makeup of the impactor.”
Thermal versus elastic heterogeneity in high‐resolution mantle circulation models with pyrolite composition: High plume excess temperatures in the lowermost mantle (2009, background): “…have remained limited as the trade-offs between thermal and chemical effects have not allowed an unequivocal identification of the cause of heterogeneities both for the upper [Cammarano et al., 2003] and the lower mantle [Deschamps and Trampert, 2004; Mattern et al., 2005; Matas et al., 2007].”
Stagnant slab : A review (2009, result): “The value of R is then 2.0, which is, according to Schmid et al. (2006), consistent with the theoretical estimate of Cammarano et al. (2003), The P, S and bulk sound velocity anomalies in the transition zone can be, according to Schmid et al. (2006), consistently explained by the temperatures of…”
Radiogenic heat production, thermal regime and evolution of continental crust (2013, background): “The velocity of P and S waves in the upper mantle depends on composition and temperature (Cammarano et al., 2003).”
Thermodynamics of mantle minerals – I. Physical properties (2005, background): “Hybrid models, where a model of physical properties is supplemented by an account of phase equilibria from an independent source, are not self-consistent (Ita & Stixrude 1992; Cammarano et al. 2003; Hacker et al. 2003).”
Mineralogy and elasticity of the oceanic upper mantle: Origin of the low‐velocity zone (2005, methodology): “…models are thus not self-consistent: A model of physical properties is supplemented with an account of phase equilibria from an independent source such as a tabular or graphical summary of experimental data [Ita and Stixrude, 1992; Vacher et al., 1998; Cammarano et al., 2003; Hacker et al., 2003].”
Multiscale full waveform inversion (2013, unknown): “Viscoelastic dissipation in the Earth, typically parametrized in terms of Q or its inverse, is mostly inferred from the frequency-dependent amplitudes of seismic waves (e.g. Canas & Mitchell 1978; Flanagan & Wiens 1998; Kennett & Abdullah 2011).”
Reconciling dynamic and seismic models of Earth's lower mantle: The dominant role of thermal heterogeneity (2012, background): “…are strongly influenced by (different) uncertainties in shear and compressional wave speed anomalies and their one-dimensional reference profiles (e.g. Karato and Karki, 2001; Ritsema and van Heijst, 2002; Cammarano et al., 2003; Brodholt et al., 2007; Cobden et al., 2009; Della Mora et al., 2011).”
Geodynamics of the Yellowstone hotspot and mantle plume: Seismic and GPS imaging, kinematics, and mantle flow (2009, methodology): “To assess the dynamic properties of the imaged plume, we employed the thermodynamic models of Cammarano et al. (2003) and Cammarano and Romanowicz (2007) with the constraints of our velocity and seismic attenuation models.”
Influence of phase transformations on lateral heterogeneity and dynamics in Earth's mantle (2007, background): “The computed phase assemblage along the reference adiabat is in good agreement with our previous results and many previous studies (Ita and Stixrude, 1992; Cammarano et al., 2003; Stixrude and Lithgow-Bertelloni, 2005b) (Fig.”
GyPSuM: A joint tomographic model of mantle density and seismic wave speeds (2010, background): “This bias towards the lowest acceptable values in the upper mantle (based on the range for the 1300°C adiabat calculations in [Cammarano et al. 2003]) is most likely a product of the combined effects of cratons and high-temperature zones that both require lowered scaling values to account for iron d”