ArticleScience advances2023
Transition from carbonatitic magmas to hydrothermal brines: Continuous dilution or fluid exsolution?
Article in Science advances, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
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Who cites it
5 citing papers in PubMed, 27 citations in OpenAlex.
- Formation of giant carbonatite rare earth deposits controlled by deep-seated magma chambers.Nature communications · 2026Article
- Reaction-driven magmatic crystallisation at the Maoniuping carbonatite.Nature communications · 2025Article
- Paleozoic carbonatites controlled rare-earth-elements mineralization at Bayan Obo.Science advances · 2025Article
- Transient crystallisation of rare earth carbonates during the hydrothermal oxidation of siderite.RSC advances · 2024Article
- Experimental evidence reveals the mobilization and mineralization processes of rare earth elements in carbonatites.Science advances · 2024Article
Corrections and comments
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Authors and funding
5 authors at 3 institutions in 1 country.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Carbonatites are the most important primary sources for the rare earth elements (REEs). While fractional crystallization of carbonate minerals results in the enrichment of volatiles, alkalis, and REEs in the remaining melts, the transition from carbonatitic magmas to hydrothermal brines remains unclear. Here, we investigated the pressure-temperature-composition (
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Registered trials
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