Results 261 to 270 of about 6,881 (288)
Tidally driven remelting around 4.35 billion years ago indicates the Moon is old. [PDF]
Nimmo F, Kleine T, Morbidelli A.
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Internal Heat Flux and Energy Imbalance of Uranus
Abstract With its extreme axial tilt, Uranus' radiant energy budget (REB) and internal heat flux remain among the most intriguing mysteries in our solar system. By combining observations with modeling, we present the global REB over a complete orbital period (1946–2030), revealing significant seasonal variations.
Xinyue Wang+15 more
wiley +1 more source
Investigations into the Diversity and Distribution of tRNA and Phylogenetics of Translation Factors in Amoebozoa-Infecting <i>Nucleocytoviricota</i>. [PDF]
Moreira TIR+6 more
europepmc +1 more source
Manifesto: challenging the standard cosmological model. [PDF]
Binney J+3 more
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Giant planet formation: a first classification of isothermal protoplanetary equilibria
B. Pečnik, G. Wuchterl
openalex
Perspectives on the physics of late-type stars from beyond low earth orbit, the moon and mars. [PDF]
Mathur S, Santos ÂRG.
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The giant planets contain the bulk of the angular momentum of the solar system and the dominant mass among the planets. The magnetosphere of the Jovian system dwarfs the Sun in size. Jupiter, Saturn, and Neptune radiate considerably more energy than they receive from the Sun.
Eugene F. Milone, William J. F. Wilson
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Interiors of the Giant Planets [PDF]
Unlike the terrestrial planets, the giant planets—Jupiter, Saturn, Uranus, and Neptune—have retained large amounts of the carbon, nitrogen, and oxygen compounds that were present in their zone of formation. A smaller fraction of the available hydrogen and helium was retained. The distribution and relative amounts of these components in the interiors of
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