S40RTS: A degree-40 shear-velocity model for the mantle from new Rayleigh wave dispersion, teleseismic traveltime and normal-mode splitting function measurements

By J. Ritsema, A. Deuss, H. V. Heijst, J. Woodhouse. 2011

1,081 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/81bff823e917118086c8fec6243d632b5121f67d

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

MASS–RADIUS RELATION FOR ROCKY PLANETS BASED ON PREM (2015, background): “The uncertainties of the fit are similar to the intrinsic uncertainty of PREM in ρ of ∼ 1% (See (Ricolleau et al. 2009) and (Ritsema et al. 2011) and Figure 3 of (Huang et al. 2011)).”
Joint inversion for global isotropic and radially anisotropic mantle structure including crustal thickness perturbations (2015, methodology): “S362WMANI +M [Moulik and Ekström, 2014], SAW642ANb [Panning et al., 2010], S40RTS [Ritsema et al., 2011], and SAVANI [Auer et al., 2014] are whole-mantle S velocity models based on surface wave and body wave data, while SEMum2 [French et al., 2013] and SL2013sv [Schaeffer and Lebedev, 2013] are…”
Morphology of seismically slow lower-mantle structures (2016, methodology): “S40RTS: a degree-40 shear-velocity model for the mantle from new Rayleigh wave dispersion, teleseismic traveltime and normal-mode splitting function, Geophys.”
The relationship between shear wave velocity, temperature, attenuation and viscosity in the shallow part of the mantle (2013, methodology): “The parameters obtained from AR for PM_v2_2012 and S40RTS (Ritsema et al., 2011), and from both AR and V s for three other recently published tomographic models largely based on surface waves: S362ANI (Kustowski et al., 2008), SAW642ANb (Panning et al., 2010) and SEMum (Lekić and Romanowicz,…”
Savani: A variable resolution whole‐mantle model of anisotropic shear velocity variations based on multiple data sets (2014, methodology): “…Panning et al., 2010; Kustowski et al., 2008; Nettles and Dziewoński, 2008; French et al., 2013; Boschi et al., 2004], spherical harmonics [e.g., Ritsema et al., 2011; Ferreira et al., 2010], triangles and layers [e.g., Schaeffer and Lebedev, 2013], tetrahedra [e.g., Sigloch, 2011], wavelets…”
TX2019slab: A New P and S Tomography Model Incorporating Subducting Slabs (2019, background): “, 2013), and Figure 8 compares S models (French & Romanowicz, 2014; Moulik & Ekström, 2014; Ritsema et al., 2011).”
SP12RTS: a degree-12 model of shear- and compressional-wave velocity for Earth's mantle (2016, methodology): “We use the inversion framework of the shear-wave velocity models S20RTS (Ritsema et al. 1999, RHW99 from hereon), S20RTSb (Ritsema et al. 2004, RHW04 from hereon) and S40RTS (Ritsema et al. 2011, RDHW11 from hereon).”
Reconciling dynamic and seismic models of Earth's lower mantle: The dominant role of thermal heterogeneity (2012, methodology): “Furthermore, we account for limited tomographic resolution when comparing to the tomographic model S40RTS (Ritsema et al., 2007, 2011).”
Whole-mantle radially anisotropic shear velocity structure from spectral-element waveform tomography (2014, methodology): “…global studies, including both whole-mantle (e.g. Panning & Romanowicz 2006; Simmons et al. 2006, 2010; Houser et al. 2008; Kustowski et al. 2008; Ritsema et al. 2011) and upper-mantle models (e.g. Lekić & Romanowicz 2011a; Debayle & Ricard 2012; Schaeffer & Lebedev 2013), with some claiming…”
Global adjoint tomography: first-generation model (2016, methodology): “Here, we present a comparison with S40RTS (Ritsema et al. 2011), a recent degree-40 global model.”