Asthenospheric low-velocity zone consistent with globally prevalent partial melting
Author:
Funder
National Science Foundation
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://www.nature.com/articles/s41561-022-01116-9.pdf
Reference83 articles.
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2. Priestley, K. & McKenzie, D. The relationship between shear wave velocity, temperature, attenuation and viscosity in the shallow part of the mantle. Earth Planet. Sci. Lett. 381, 78–91 (2013).
3. Gung, Y., Panning, M. & Romanowicz, B. Global anisotropy and the thickness of continents. Nature 422, 707–711 (2003).
4. Burgos, G. et al. Oceanic lithosphere–asthenosphere boundary from surface wave dispersion data. J. Geophys. Res. Solid Earth 119, 1079–1093 (2014).
5. Beghein, C., Yuan, K., Schmerr, N. & Xing, Z. Changes in seismic anisotropy shed light on the nature of the Gutenberg discontinuity. Science 343, 1237–1240 (2014).
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