Global 3D model of mantle attenuation using seismic normal modes
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DOI: 10.1038/s41586-024-08322-y
Abstract: Seismic tomographic models based only on wave velocities have limited ability to distinguish between a thermal or compositional origin for Earth’s 3D structure1. Complementing wave velocities with attenuation observations can make that distinction, which is… read more here.
Keywords: grain size; model mantle; model; global model ... See more keywords