An exogenic to endogenic thermal transition on Earth 3.9 billion years ago

An exogenic to endogenic thermal transition on Earth 3.9 billion years ago

Abstract On Earth, the primary driver of crustal magmatism is generally viewed as endogenic, a manifestation of loss of primordial and radiogenic heat from the interior. However, a much higher impact flux during the Hadean and earliest Archean eons would have significantly contributed to the crustal...

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Bibliographic Details
Main Authors: Christopher L. Kirkland, Janne Liebmann, Hamed Gamaleldien, Hugo K. H. Olierook, Maximilian Dröllner, Tim Johnson, Craig O’Neill, Axel K. Schmitt
Format: Article
Language:English
Published: Nature Portfolio 2025-07-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02575-9
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