Evolution of Pluto's Impact‐Deformed Ice Shell Below Sputnik Planitia Basin
Author:
Affiliation:
1. Department of Geophysics Faculty of Mathematics and Physics Charles University Prague Czech Republic
2. Mathematical Institute of Charles University Faculty of Mathematics and Physics Charles University Prague Czech Republic
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022JE007221
Reference46 articles.
1. III. On the computation of the effect of the attraction of mountain-masses, as disturbing the apparent astronomical latitude of stations in geodetic surveys
2. Convection in ice I shells and mantles with self-consistent grain size
3. Evidence for a hot start and early ocean formation on Pluto
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1. Thickness of Pluto's Ice Shell from elastic deformation of the Sputnik Planitia forebulge: Response to infill load or vestige of impact event?;Earth and Planetary Science Letters;2024-11
2. Sputnik Planitia as an impactor remnant indicative of an ancient rocky mascon in an oceanless Pluto;Nature Astronomy;2024-04-15
3. The role of Pluto's ocean's salinity in supporting nitrogen ice loads within the Sputnik Planitia basin;Icarus;2024-04
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