Construct · 1 fields · 1 citations

depleted mantle model age: a standalone construct

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Geochemistry

the time when a crustal sample's isotope ratio last matched a depleted mantle reservoir, read as its crust formation age.

In geochemistry, depleted mantle model age refers to the time when a crustal sample's isotope ratio last matched a depleted mantle reservoir, read as its crust formation age. This meaning comes from DePaolo (1981) in Nature.[1]

Unit
Recovery means
Measured by

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Nearby constructs

model3 fields · 3 citationsjingle · one word, three constructs reservoir1 fields · 1 citationsanchor · a standalone construct sample3 fields · 3 citationsjingle · one word, three constructs

References

DePaolo, D. J. (1981). Neodymium isotopes in the Colorado Front Range and crust–mantle evolution in the Proterozoic. Nature, 291(5812), 193-196. https://doi.org/10.1038/291193a0

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