Shallow mantle temperatures under Europe from P and S wave tomography

By S. Goes, R. Govers, Pierre Vacher. 2000

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In Geophysics

Citations in the corpus

The thermal structure of subduction zone back arcs (2004, methodology): “In addition, both southern Europe and Asia are characterized by low upper mantle seismic velocities from surface wave tomography and Pn velocity studies [Ritzwoller and Levshin, 1998; Ritzwoller et al., 2002].”
Complex subduction and small-scale convection revealed by body-wave tomography of the western United States upper mantle (2010, background): “Mantle temperature variations are predicted to produce δlnVS/δlnVP of 1.2–2 (Anderson et al., 1992; Goes et al., 2000) depending primarily on the assumed attenuation structure.”
Thermodynamic constraints on seismic inversions (2004, methodology): “wave velocity (km s −1 ) 300 200 100 0 depth (km) 4 5”
Joint inversion of seismic and gravity data for lunar composition and thermal state (2007, background): “Goes et al. 2000; Cammarano et al. 2003; Deschamps & Trampert 2004; Godey et al. 2004; Shapiro & Ritzwoller 2004; Trampert et al. 2004; Mattern et al. 2005).”
The thermal structure of the lithosphere from shear wave velocities (2006, background): “'s [38] expression and Shapiro and Ritzwoller's [39, and personal communication] constants (Fig.”
The relationship between shear wave velocity, temperature, attenuation and viscosity in the shallow part of the mantle (2013, background): “Goes et al. (2000) and Faul and Jackson (2005) extrapolated the results from laboratory experiments to mantle conditions to estimate the temperature from the pressure and V s .”
Cooling history of the Pacific lithosphere (2003, methodology): “Both issues have been increasingly ameliorated in recent years due to the growth of the global seismic network and advances in the theory of thermoelasticity [15].”
The continental lithosphere: Reconciling thermal, seismic, and petrologic data (2009, background): “The relative difference in the ΔVs amplitudes between the CLM of the East European Platform (which, along the entire profile, remained tectonically undisturbed since the Paleoproterozoic) and the Karelian Province of the Baltic Shield (where kimberlite magmatism followed pre-existing lithosphere wea”
Inferring surface heat flux distributions guided by a global seismic model: particular application to Antarctica (2004, background): “The merit derives from the fact that the vertical seismic velocity gradient in the mantle is related to the temperature gradient which controls the mantle component of heat flow [8,15–17].”
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.”
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].”
Influence of phase transformations on lateral heterogeneity and dynamics in Earth's mantle (2007, background): “…elastic part of the velocity on temperature as required by the third law, whereas Cammarano et al. (2003), and many other previous studies of the upper mantle and transition zone (Vacher et al., 1998; Goes et al., 2000), assume a linear dependence from ambient temperature to mantle temperatures.”
Deep Europe today: geophysical synthesis of the upper mantle structure and lithospheric processes over 3.5 Ga (2006, methodology): “…thickness during the Variscan orogeny was probably between 40 and 50 km, implying a ca. 40-50 km growth of the lithosphere by thermal cooling over 200-300 Ma. Regional P- and S-wave tomographic models have been recently used to assess upper mantle temperatures in western Europe (Goes et al. 2000).”