Evidence for a kilometre-scale seismically slow layer atop the core-mantle boundary from normal modes
Abstract
Geodynamic modelling and seismic studies have highlighted the possibility that a thin layer of low seismic velocities, potentially molten, may sit atop the core-mantle boundary but has thus far eluded detection. In this study we employ normal modes, an independent data type to body waves, to assess the visibility of a seismically slow layer atop the core-mantle boundary to normal mode centre frequencies. Using forward modelling and a dataset of 353 normal mode observations we find that some centre frequencies are sensitive to one-dimensional kilometre-scale structure at the core-mantle boundary. Furthermore, a global slow and dense layer 1 - 3 km thick is better-fitting than no layer. The well-fitting parameter space is broad with a wide range of possible seismic parameters, which precludes inferring a possible composition or phase. Our methodology cannot uniquely detect a layer in the Earth but one should be considered possible and accounted for in future studies.
Keywords
Cite
@article{arxiv.2311.15862,
title = {Evidence for a kilometre-scale seismically slow layer atop the core-mantle boundary from normal modes},
author = {Stuart Russell and Jessica C. E. Irving and Lisanne Jagt and Sanne Cottaar},
journal= {arXiv preprint arXiv:2311.15862},
year = {2023}
}