Cargando…
Widespread impact-generated porosity in early planetary crusts
NASA’s Gravity Recovery and Interior Laboratory (GRAIL) spacecraft revealed the crust of the Moon is highly porous, with ~4% porosity at 20 km deep. The deep lying porosity discovered by GRAIL has been difficult to explain, with most current models only able to explain high porosity near the lunar s...
Autores principales: | Wiggins, Sean E., Johnson, Brandon C., Collins, Gareth S., Jay Melosh, H., Marchi, Simone |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9381781/ https://www.ncbi.nlm.nih.gov/pubmed/35974008 http://dx.doi.org/10.1038/s41467-022-32445-3 |
Ejemplares similares
-
Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites
por: Chernonozhkin, S. M., et al.
Publicado: (2021) -
Porosity evolution at the brittle-ductile transition in the continental crust: Implications for deep hydro-geothermal circulation
por: Violay, M., et al.
Publicado: (2017) -
Early porosity generation in organic-sulfur-rich mudstones
por: Knapp, Levi J., et al.
Publicado: (2023) -
Early oxidation of the martian crust triggered by impacts
por: Deng, Zhengbin, et al.
Publicado: (2020) -
Crusted scabies
por: Lyons, D., et al.
Publicado: (2023)