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Updated: May 11, 2026

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas
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火星,地球,そして月のスーパーコンドリティックSm/Nd比

Guillaume Caro1, Bernard Bourdon, Alex N Halliday

  • 1Laboratoire Géochimie et Cosmochimie Institut de Physique du Globe de Paris-Université Denis Diderot, 4 place Jussieu, 75252 Paris Cedex 05, France. caro@crpg.cnrs-nancy.fr

Nature
|March 21, 2008
PubMed
まとめ

ネオジム-142 (142Nd) の同位体分析により,火星は地球と同様に非コンドリート組成を有しており,初期の惑星の分化を示していることが明らかになった. 火星の隕石は,マントルの分化が太陽系から4000万年後に起こったことを示唆しています.

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