Data sets for “The Emperor-Hawaiian chain magmatism: 80 Ma of isothermal melting”

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Authors: Nikolai Nekrylov, Vadim Kamenetsky
Cited by: 1

Abstract

By analyzing olivine-hosted Cr-spinel and melt inclusions from primitive lavas, we find that the Hawaiian plume has maintained a consistently high potential temperature (~1450oC) since the Early Cretaceous, significantly hotter than the surrounding mantle.

Publication details

Journal / source
Figshare
Publication date
1 September 2026
Document type
Dataset