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   https://doi.org/10.3847/1538-4357/abce57  

   O’Dell, C. R. ; Abel, N. P. ; Ferland, G. J. ( February 2021 , The Astrophysical Journal)

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2. A sporadic low-velocity layer atop the 410 km discontinuity beneath the Pacific Ocean: Low-Velocity Layer Atop the Pacific 410

   https://doi.org/10.1002/2017JB014100  

   Wei, S. Shawn ; Shearer, Peter M. ( July 2017 , Journal of Geophysical Research: Solid Earth)
3. Instability of the African large low-shear-wave-velocity province due to its low intrinsic density

   https://doi.org/10.1038/s41561-022-00908-3  

   Yuan, Qian ; Li, Mingming ( April 2022 , Nature Geoscience)
4. Asthenospheric low-velocity zone consistent with globally prevalent partial melting

   https://doi.org/10.1038/s41561-022-01116-9  

   Hua, Junlin ; Fischer, Karen M. ; Becker, Thorsten W. ; Gazel, Esteban ; Hirth, Greg ( February 2023 , Nature Geoscience)

   The asthenosphere plays a fundamental role in present-day plate tectonics as its low viscosity controls how convection in the mantle below it is expressed at the Earth’s surface above. The origin of the asthenosphere, including the role of partial melting in reducing its viscosity and facilitating deformation, remains unclear. Here we analysed receiver-function data from globally distributed seismic stations to image the lower reaches of the asthenospheric low-seismic-velocity zone. We present globally widespread evidence for a positive seismic-velocity gradient at depths of ~150 km, which represents the base of a particularly low-velocity zone within the asthenosphere. This boundary is most commonly detected in regions with elevated upper-mantle temperatures and is best modelled as the base of a partially molten layer. The presence of the boundary showed no correlation with radial seismic anisotropy, which represents accumulated mantle strain, indicating that the inferred partial melt has no substantial effect on the large-scale viscosity of the asthenosphere. These results imply the presence of a globally extensive, partially molten zone embedded within the asthenosphere, but that low asthenospheric viscosity is controlled primarily by gradual pressure and temperature variations with depth. 

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5. Investigating ultra-low velocity zones in the southern hemisphere using an Antarctic dataset

   https://doi.org/10.1016/j.epsl.2020.116142  

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