High Ni and low Mn/Fe in olivine phenocrysts of the Karoo meimechites do not reflect pyroxenitic mantle sources
Author:
Funder
University of Helsinki
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference56 articles.
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3. 186Os–187Os and highly siderophile element abundance systematics of the mantle revealed by abyssal peridotites and Os-rich alloys;Day;Geochim. Cosmochim. Acta,2017
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