Non‐linear global P‐wave tomography by iterated linearized inversion

By H. Bijwaard, W. Spakman. 2000

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Wavefront healing: a banana–doughnut perspective (2001, background): “D structure (e.g. Bijwaard & Spakman 2000;Widiyantoro et al. 2000).”
Global adjoint tomography: first-generation model (2016, background): “…& Toksöz 1977), many models of the mantle have been published based on various types of data, such as body-wave arrival times (e.g. Dziewoński 1984; Bijwaard & Spakman 2000; Boschi & Dziewoński 2000; Zhou et al. 2006), surface-wave dispersion (e.g. Trampert & Woodhouse 1995; Ekström et al.…”
P‐ and S‐velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data (2009, background): “However, this fast anomaly is attenuated between 50 and 100 km (cross-sections 4), which provides evidence for an extension of the gap detected in the central-southern Apennines to this area (Bijwaard & Spakman 2000).”
Finite‐frequency tomography using adjoint methods—Methodology and examples using membrane surface waves (2007, methodology): “Bijwaard & Spakman (2000) performed 3-”
Deep Europe today: geophysical synthesis of the upper mantle structure and lithospheric processes over 3.5 Ga (2006, methodology): “The vertical resolution is 50-100 km for the upper 250 km and coverage disappears at deeper levels; the lateral resolution does not exceed 500-1000 km. (c) As (a) for 265 km depth (based on the model of Bijwaard & Spakman 2000).”