Melts generated at the Martian core–mantle boundary would be strongly enriched in iron and have high densities favouring the formation of a molten silicate layer previously suggested from InSight seismic data, according to experimental constraints…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
- Earth–Moon and Solar System history recorded in Mesoproterozoic Grand Canyon strata
- Experimental constraints on a long-lived magma layer at the Martian core–mantle boundary
- Rapid submarine caldera collapse during the 2022 climactic eruption of Hunga volcano (Tonga)
- Maximum earthquake magnitude unlikely to be controlled by subduction interface roughness
- A strengthening yet less extreme Atlantic–European jet during winter
- Martian Hadley circulation divides the atmosphere and connects the poles
- Multilayer soil moisture deficit amplifies drought impacts on global ecosystems
- Publisher Correction: Hadley circulation drives material isolation and pole-to-pole teleconnection on Mars
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