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Comment on “Discovery of davemaoite, CaSiO₃-perovskite, as a mineral from the lower mantle”

Walter, Michael J; Kohn, Simon C; Pearson, D Graham; Shirey, Steven B; Speich, Laura; Stachel, Thomas; Thomson, Andrew R; (2022) Comment on “Discovery of davemaoite, CaSiO₃-perovskite, as a mineral from the lower mantle”. Science , 376 (6593) pp. 1-4. 10.1126/science.abo0882. Green open access

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Abstract

Tschauner et al. (Reports, 11 November 2021, p. 891) present evidence that diamond GRR-1507 formed in the lower mantle. Instead, the data support a much shallower origin in cold, subcratonic lithospheric mantle. X-ray diffraction data are well matched to phases common in microinclusion-bearing lithospheric diamonds. The calculated bulk inclusion composition is too imprecise to uniquely confirm CaSiO₃ stoichiometry and is equally consistent with inclusions observed in other lithospheric diamonds.

Type: Article
Title: Comment on “Discovery of davemaoite, CaSiO₃-perovskite, as a mineral from the lower mantle”
Open access status: An open access version is available from UCL Discovery
DOI: 10.1126/science.abo0882
Publisher version: https://www.science.org/toc/science/0/0
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
UCL classification: UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL
URI: https://discovery-pp.ucl.ac.uk/id/eprint/10148031
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