Subducted carbonates not required: Deep mantle melting explains stable Ca isotopes in kimberlite magmas
Author:
Funder
Swiss National Science Foundation
National Natural Science Foundation of China
ETH Zurich
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference165 articles.
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2. Hydrothermal alteration of kimberlite by convective flows of external water;Afanasyev;Contrib. Miner. Petrol.,2014
3. Calcium isotope fractionation during the partial dissolution of artificial calcite;Alkhatib;J. Sea Res.,2022
4. Calcium isotopes (δ44/40Ca) in MPI-DING reference glasses, USGS rock powders and various rocks: Evidence for Ca isotope fractionation in terrestrial silicates;Amini;Geostand. Geoanal. Res.,2009
5. Calcium isotopic evidence for the mantle sources of carbonatites;Amsellem;Sci. Adv.,2020
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