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Details

Autor(en) / Beteiligte
Titel
Lifetime of the solar nebula constrained by meteorite paleomagnetism
Ist Teil von
  • Science (American Association for the Advancement of Science), 2017-02, Vol.355 (6325), p.623-627
Ort / Verlag
United States: American Association for the Advancement of Science
Erscheinungsjahr
2017
Link zum Volltext
Quelle
American Association for the Advancement of Science
Beschreibungen/Notizen
  • A key stage in planet formation is the evolution of a gaseous and magnetized solar nebula. However, the lifetime of the nebular magnetic field and nebula are poorly constrained. We present paleomagnetic analyses of volcanic angrites demonstrating that they formed in a near-zero magnetic field (<0.6 microtesla) at 4563.5 ± 0.1 million years ago, ~3.8 million years after solar system formation. This indicates that the solar nebula field, and likely the nebular gas, had dispersed by this time. This sets the time scale for formation of the gas giants and planet migration. Furthermore, it supports formation of chondrules after 4563.5 million years ago by non-nebular processes like planetesimal collisions. The 1core dynamo on the angrite parent body did not initiate until about 4 to 11 million years after solar system formation.

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