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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| Main Authors: | , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-07-01
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| Series: | Communications Earth & Environment |
| Online Access: | https://doi.org/10.1038/s43247-025-02575-9 |
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