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