Paleomagnetic evidence for a partially differentiated ordinary chondrite parent asteroid
The textures and accretion ages of chondrites have been used to argue that their parent asteroids never differentiated. Without a core, undifferentiated planetesimals could not have generated magnetic fields through dynamo activity, so chondrites are not expected to have experienced such fields. How...
| Hauptverfasser: | , , , , , |
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| Format: | Artikel |
| Sprache: | English |
| Veröffentlicht: |
American Geophysical Union (AGU)
2020
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| Online Zugang: | https://hdl.handle.net/1721.1/125340 |