Xenolith Constraints on “Self‐Assimilation” and the Origin of Low δ 18 O Values in Mauna Kea Basalts
Author:
Publisher
Wiley
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/9781119595007.ch6
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1. Lead isotopes reveal bilateral asymmetry and vertical continuity in the Hawaiian mantle plume
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3. Petrography and petrology of the Hawaii Scientific Drilling Project lavas: Inferences from olivine phenocryst abundances and compositions
4. High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle
5. Lithium isotope analysis of olivine by SIMS: Calibration of a matrix effect and application to magmatic phenocrysts
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