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The DOI matches its Crossref record; 52 of the 52 references it cites were found in a registry or an index.

Experimental Melting of Carbonated Peridotite at 6-10 GPa

Brey, G. P., Bulatov, V. K., Girnis, A. V., Lahaye, Y.·2007·Journal of Petrology

Abstract

Partial melting of magnesite-bearing peridotites was studied at 6^10 GPa and 1300^17008C. Experiments were performed in a multianvil apparatus using naturalmineralmixes asstartingmaterial placed into olivine containers and sealed in Pt capsules. Partial melts originated within the peridotite layer, migrated outside the olivine container and formed pools of quenched melts along the wall of the Pt capsule. This allowed the analysis of even small melt fractions. Iron loss was not a problem, because the platinum near the olivine container became saturated in Fe as a result of the reaction Fe2SiO4 OlFeFe^Pt alloyþFeSiO3OpxþO2.This reaction led to a gradual increase in oxygen fugacity within the capsules as expressed, for example, in high Fe3þ in garnet. Carbonatitic to kimberlite-like melts were obtained that coexist with olivineþ orthopyroxeneþ garnet clinopyroxenemagnesite depending on P^T conditions.

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Metadata

Authors
Brey, G. P., Bulatov, V. K., Girnis, A. V., & Lahaye, Y.
Venue
Journal of Petrology
Published
2007-10-11
Volume
49
Issue
4
Pages
797-821
ISSN
  • 0022-3530 (ISSN-L)
  • 1460-2415
OpenAlex
W2152550713
Cited by
316
References
52
FWCI
10.45
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Experimental Melting of Carbonated Peridotite at 6-10 GPa. https://app.cochat.ai/papers/10.1093/petrology/egn002
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Brey, G. P., Bulatov, V. K., Girnis, A. V., & Lahaye, Y. (2007). Experimental Melting of Carbonated Peridotite at 6-10 GPa. Journal of Petrology. https://doi.org/10.1093/petrology/egn002

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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