Global variability of transition zone thickness

136 citations recorded by the source corpus.

How researchers see this paper

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

An anisotropic shear velocity model of the Earth's mantle using normal modes, body waves, surface waves and long-period waveforms (2014, methodology): “Therefore, S362ANI+M shows depressions in the 650- km discontinuity beneath the slab-like anomalies that are in broad agreement with other studies (Shearer & Masters 1992; Flanagan & Shearer 1998; Gu & Dziewoński 2002; Houser et al. 2008a; Kustowski et al. 2008).”
A global study of transition zone thickness using receiver functions (2006, methodology): “and Shearer, 1998; Gu et al., 1998; Gu and Dziewonski, 2002 ] indicates that the results are robust.”
Anisotropic shear‐wave velocity structure of the Earth's mantle: A global model (2008, unknown): “This spectral change has been reported previously by Gu et al. [2001a], who found longwavelength anomalies in the entire upper mantle to be much stronger than in the lower mantle.”