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...

Бүрэн тодорхойлолт

Номзүйн дэлгэрэнгүй
Үндсэн зохиолчид: Maurel, Clara, Bryson, James F. J., Shah, Jay, Chopdekar, Rajesh V., T. Elkins‐Tanton, Linda, A. Raymond, Carol, Weiss, Benjamin P.
Бусад зохиолчид: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Формат: Өгүүллэг
Хэл сонгох:English
Хэвлэсэн: American Geophysical Union (AGU) 2022
Онлайн хандалт:https://hdl.handle.net/1721.1/140396