Reevaluating the evidence for a Hadean-Eoarchean dynamo

Publication Year
2020
Abstract

The time of origin of the geodynamo has important implications for the thermal evolution of the planetary interior and the habitability of early Earth. It has been proposed that detrital zircon grains from Jack Hills, Western Australia, provide evidence for an active geodynamo as early as 4.2 billion years (Ga) ago. However, our combined paleomagnetic, geochemical, and mineralogical studies on Jack Hills zircons indicate that most have poor magnetic recording properties and secondary magnetization carriers that postdate the formation of the zircons. Therefore, the existence of the geodynamo before 3.5 Ga ago remains unknown.

Journal
Science Advances
Volume
6
Issue
15
Pages
1-9
Date Published
04/2020
ISSN Number
ISSN 2375-2548
Other Numbers
67Maloof
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