Nature Geoscience, Published online: 17 June 2026; doi:10.1038/s41561-026-02018-w
Heat flux across the core–mantle boundary is laterally variable, and heat may flow into the core beneath hot piles of dense material such as large low-shear-wave-velocity provinces, according to mantle thermochemical convection models…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
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