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Xenolith Constraints on the Mantle Potential Temperature and Thickness of Cratonic Roots Through Time

Abstract The temperature of the convecting mantle and thickness of the lithosphere control many of Earth's processes. However, there is disagreement regarding the evolution of these quantities through time. We use a global data set of mantle xenoliths and xenocrysts to construct paleogeotherms at di...

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Hlavní autoři: Z. J. Sudholz, A. Copley
Médium: Artigo
Jazyk:Inglês
Vydáno: Wiley 2025-01-01
Edice:Geophysical Research Letters
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On-line přístup:https://doi.org/10.1029/2024GL112851
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