A Long‐Lived Planetesimal Dynamo Powered by Core Crystallization
The existence of numerous iron meteorite groups indicates that some planetesimals underwent melting that led to metal-silicate segregation, sometimes producing metallic cores. Meteorite paleomagnetic records suggest that crystallization of these cores generated dynamo magnetic fields. Here we descri...
| Үндсэн зохиолчид: | , , , , , , |
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| Бусад зохиолчид: | |
| Формат: | Өгүүллэг |
| Хэл сонгох: | English |
| Хэвлэсэн: |
American Geophysical Union (AGU)
2022
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| Онлайн хандалт: | https://hdl.handle.net/1721.1/140396 |