Mantle depletion recorded by olivine and plagioclase megacrysts in oceanic basalts
(2024)
Journal Article
Burton, K., Parkinson, I., & Neave, D. (in press). Mantle depletion recorded by olivine and plagioclase megacrysts in oceanic basalts. Geochemical perspectives letters, 29, 9-13. https://doi.org/10.7185/geochemlet.2405
Earth’s oceanic crust is largely formed by melting of the upper mantle where it upwells beneath mid-ocean ridges, providing a geographically widespread elemental and isotopic ‘sample’ of Earth’s interior. Radiogenic isotope variations in oceanic basa... Read More about Mantle depletion recorded by olivine and plagioclase megacrysts in oceanic basalts.