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Provenance of the terrestrial planets

Geochimica et Cosmochimica Acta, 1994
Earlier work on the simultaneous accumulation of the asteroid belt and the terrestrial planets is extended to investigate the relative contribution to the final planets made by material from different heliocentric distances. As before, stochastic variations intrinsic to the accumulation processes lead to a variety of final planetary configurations, but
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Formation of the terrestrial planets

Earth, Moon, and Planets, 1994
The early phases of formation in the inner solar system were dominated by collisions and short-range dynamical interactions among planetesimals. But the later phases, which account for most of the differences among planets, are unsure because the dynamics are more subtle. Jupiter’s influence became more important, leading to drastic clearing out of the
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Structure of the Terrestrial Planets

Nature, 1973
Recent reviews (cf. Runcorn, 1968; or Cook, 1972, 1975) on the structure of the planets omit reference to the phase-change hypothesis for the nature of the terrestrial core, despite that numerous prior predictions of the theory based on this hypothesis have subsequently been borne out as correct.
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The Terrestrial Planets

1979
The terrestrial planets possess markedly different intrinsic densities (Table 6.3), implying the existence of corresponding differences in chemical composition. Possible reasons for the compositional differences which were considered in Section 6.5, involved (a) fractionation of metallic iron from silicates in the nebula prior to accretion, and/or (b ...
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Making More Terrestrial Planets

Icarus, 2001
The results of 16 new 3D N-body simulations of the final stage of the formation of the terrestrial planets are presented. These Nbody integrations begin with 150‐160 lunar-to-Mars size planetary embryos, with semi-major axes 0.3< a < 2.0 AU, and include perturbations from Jupiter and Saturn.
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The Strangest Terrestrial Planet

Science, 2012
NASA's MESSENGER mission previously revealed that Mercury has a volcanic crust; now it finds evidence for an inner “anticrust.”
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Terrestrial planets

2015
Vadym Kaydash   +3 more
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Climates of terrestrial planets

2016
Suppose we detect a planet half the size of Venus orbiting a 5 billion year old M-type star at 0.5 AU. To our surprise the planet has detectable radiation belts. How might the planet's climate and surface habitability differ from that of Venus? The prospect that the scientific community might be faced in the next decade or two with questions like the
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Life and death in the soil microbiome: how ecological processes influence biogeochemistry

Nature Reviews Microbiology, 2022
Noah W Sokol   +2 more
exaly  

A planet within the debris disk around the pre-main-sequence star AU Microscopii

Nature, 2020
Peter Plavchan   +2 more
exaly  

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