Iron meteorites as remnants of planetesimals formed in the terrestrial planet region
about
Rethinking early Earth phosphorus geochemistryLunar formation. Dating the Moon-forming impact event with asteroidal meteorites.Early inner solar system origin for anomalous sulfur isotopes in differentiated protoplanets.An anomalous basaltic meteorite from the innermost main belt.A potential hidden layer of meteorites below the ice surface of AntarcticaIsotopes as tracers of the sources of the lunar material and processes of lunar origin.Age of Jupiter inferred from the distinct genetics and formation times of meteorites.Stochastic late accretion to Earth, the Moon, and MarsThe empty primordial asteroid belt.Evidence for a dynamo in the main group pallasite parent body.Solar System FormationMercury and other iron-rich planetary bodies as relics of inefficient accretionChallenges in planet formationDid Jupiter's core form in the innermost parts of the Sun's protoplanetary disc?Solar System evolution from compositional mapping of the asteroid beltBody-Centered Cubic Iron-Nickel Alloy in Earth's Core
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Iron meteorites as remnants of planetesimals formed in the terrestrial planet region
description
2006 nî lūn-bûn
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2006年の論文
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name
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region
@en
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region.
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type
label
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region
@en
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region.
@nl
prefLabel
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region
@en
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region.
@nl
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P1476
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region
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David Nesvorný
David P O'Brien
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10.1038/NATURE04536
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P577
2006-02-01T00:00:00Z
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P6179
1003954760