An experimental study of dissolution–reprecipitation in fluorapatite: fluid infiltration and the formation of monazite
By D. Harlov, R. Wirth, H. Förster. 2005
378 citations recorded by the source corpus.
Subfields: Biomedical Engineering, Electronic, Optical and Magnetic Materials, Geophysics
View Paper: https://www.semanticscholar.org/paper/df2be1b4d484994b00975cd8b5607289f9260945
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In Biomedical Engineering
In Electronic, Optical and Magnetic Materials
In Geophysics
Citations in the corpus
- Trace metal nanoparticles in pyrite (2011, background): “This process would dissolve and redistribute any elements that were present in trace concentrations in the host mineral and it has been shown to account for inclusions of monazite during dissolution–reprecipitation of fluorapatite (Harlov et al., 2005).”
- Mineral Replacement Reactions (2009, background): “In a separate set of hydrothermal experiments using a wide range of fluid compositions at temperatures between 300 and 900 °C, Harlov et al. (2003, 2005) determined the conditions under which monazite inclusions could be induced to form from the LREE-enriched Durango fluorapatite.”