The thermal evolution of planetesimals during accretion and differentiation: consequences for dynamo generation by thermally-driven convection

The thermal evolution of planetesimals during accretion and differentiation: consequences for dynamo generation by thermally-driven convection

The meteorite paleomagnetic record indicates that differentiated (and potentially, partially differentiated) planetesimals generated dynamo fields in the first 5-40 Myr after the formation of calcium-aluminium-rich inclusions (CAIs). This early period of dynamo activity has been attributed to therma...

Полное описание

Библиографические подробности
Главные авторы:	Dodds, K, Bryson, J, Neufeld, J, Harrison, R
Формат:	Journal article
Язык:	English
Опубликовано:	Wiley 2021

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