ArticleNature communications2022
Origin of carbonatites-liquid immiscibility caught in the act.
Article in Nature communications, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 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.
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Who cites it
7 citing papers in PubMed, 55 citations in OpenAlex.
- Formation of giant carbonatite rare earth deposits controlled by deep-seated magma chambers.Nature communications · 2026Article
- Depth-dependent anisotropy in the Earth's inner core linked to chemical stratification.Nature communications · 2025Article
- CytoSimplex: visualizing single-cell fates and transitions on a simplex.Bioinformatics (Oxford, England) · 2025Article
- Impact of Rare Earth Elements on CaCOCrystal growth & design · 2024Article
- Transition from carbonatitic magmas to hydrothermal brines: Continuous dilution or fluid exsolution?Science advances · 2023Article
- Reply to: Silica is unlikely to be soluble in upper crustal carbonatite melts.Nature communications · 2023Article
- Silica is unlikely to be soluble in upper crustal carbonatite melts.Nature communications · 2023Article
Corrections and comments
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Authors and funding
2 authors at 1 institution in 1 country.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Carbonatites are rare but worldwide occurring igneous rocks and their genesis remains enigmatic. Field studies show a close spatial but controversially debated genetic relationship with alkaline silicate rocks, and petrological and experimental studies indicate liquid immiscibility from mantle-derived magmas being one viable model for the generation of carbonatites. However, unaltered carbonatitic melts are rare and the composition of primary carbonate liquids and their silicate conjugates is poorly constrained. Here we show an example of primary Ca-carbonatitic melt formed by liquid immiscibility from a phonolitic magma of the Laacher See volcano (Eifel, Germany). The conjugate blebs of carbonate-silicate liquids are found in hauyne-hosted melt inclusions. The Ca-carbonatite melts are moderately alkali-rich and contain high F and Cl at elevated SiO
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