Heat Generation in Cratonic Mantle Roots—New Trace Element Constraints From Mantle Xenoliths and Implications for Cratonic Geotherms

Abstract Heat generation within the cratonic lithospheric mantle (CLM) is an important but poorly determined parameter for constructing cratonic geotherms. Direct measurement of heat producing element (HPE: K, U, and Th) concentrations in bulk‐rock samples of cratonic mantle roots—provided as xenoli...

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Detalles Bibliográficos

Principais autores:	T. McIntyre, K. Kublik, C. Currie, D. G. Pearson
Formato:	Artigo
Idioma:	Inglês
Publicado:	Wiley 2021-09-01
Series:	Geochemistry, Geophysics, Geosystems
Assuntos:	heat producing elements (K, U, and Th) mantle heat generation cratonic geotherms mantle metasomatism
Acceso en liña:	https://doi.org/10.1029/2021GC009691
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