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- S. J. Weidenschilling
- S. J. Weidenschilling, Planetary Science Institute, Tucson, AZ 85705, USA.
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- F. Marzari
- S. J. Weidenschilling, Planetary Science Institute, Tucson, AZ 85705, USA.
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- L. L. Hood
- S. J. Weidenschilling, Planetary Science Institute, Tucson, AZ 85705, USA.
説明
<jats:p>Isotopic dating indicates that chondrules were produced a few million years after the solar nebula formed. This timing is incompatible with dynamical lifetimes of small particles in the nebula and short time scales for the formation of planetesimals. Temporal and dynamical constraints can be reconciled if chondrules were produced by heating of debris from disrupted first-generation planetesimals. Jovian resonances can excite planetesimal eccentricities enough to cause collisional disruption and melting of dust by bow shocks in the nebular gas. The ages of chondrules may indicate the times of Jupiter's formation and dissipation of gas from the asteroidal region.</jats:p>
収録刊行物
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- Science
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Science 279 (5351), 681-684, 1998-01-30
American Association for the Advancement of Science (AAAS)
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詳細情報 詳細情報について
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- CRID
- 1361981469420250752
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- NII論文ID
- 30020365913
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- ISSN
- 10959203
- 00368075
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- データソース種別
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- Crossref
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