Cargando…
A partially equilibrated initial mantle and core indicated by stress-induced percolative core formation through a bridgmanite matrix
The Earth’s core formation mechanism determines the siderophile and light elements abundance in the Earth’s mantle and core. Previous studies suggest that the sink of massive liquid metal through a solid silicate mantle resulted in an unequilibrated core and the lower mantle. Here, we show that perc...
Autores principales: | Wang, Lin, Fei, Yingwei |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Association for the Advancement of Science
2023
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9931215/ https://www.ncbi.nlm.nih.gov/pubmed/36791194 http://dx.doi.org/10.1126/sciadv.ade3010 |
Ejemplares similares
-
Viscosity of bridgmanite determined by in situ stress and strain measurements in uniaxial deformation experiments
por: Tsujino, Noriyoshi, et al.
Publicado: (2022) -
Globally distributed subducted materials along the Earth’s core-mantle boundary: Implications for ultralow velocity zones
por: Hansen, Samantha E., et al.
Publicado: (2023) -
Tropical mountain ice core δ(18)O: A Goldilocks indicator for global temperature change
por: Liu, Zhengyu, et al.
Publicado: (2023) -
The combined Hf and Nd isotope evolution of the depleted mantle requires Hadean continental formation
por: Guo, Meng, et al.
Publicado: (2023) -
Slow evolution of Europa’s interior: metamorphic ocean origin, delayed metallic core formation, and limited seafloor volcanism
por: Trinh, Kevin T., et al.
Publicado: (2023)