Data sets for “The Emperor-Hawaiian chain magmatism: 80 Ma of isothermal melting”
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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 (~1450–1500<sup>o</sup>C) since the Early Cretaceous, significantly hotter than the surrounding mantle.
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figshare创建时间：
2025-03-08
