Petrological, geochemical and mineralogical characteristics of Wigu Hill carbonatite, Uluguru Mountains, Tanzania: insights into carbonatite evolution and REE mineralization
Author:
Funder
Japan International Cooperation Agency
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00126-024-01295-y.pdf
Reference65 articles.
1. Amsellem E, Schiller M, Klausen M et al (2023) Origin of carbonatites and associated silicate rocks revealed by mg triple-isotope approach. Chem Geol 636:121663. https://doi.org/10.1016/j.chemgeo.2023.121663
2. Anenburg M, Broom-Fendley S, Chen W (2021) Formation of rare earth deposits in carbonatites. Elements 17:327–332. https://doi.org/10.2138/gselements.17.5.327
3. Anenburg M, Mavrogenes JA, Frigo C, Wall F (2020) Rare earth element mobility in and around carbonatites controlled by sodium, potassium, and silica. Sci Adv 6:10
4. Appel P, Möller A, Schenk V (1998) High-pressure granulite facies metamorphism in the pan-african belt of eastern Tanzania: P-T-t evidence against granulite formation by continent collision. J Metamorph Geol 16:491–509. https://doi.org/10.1111/j.1525-1314.1998.00150.x
5. Araoka D, Simandl GJ, Paradis S et al (2022) Formation of the Rock Canyon Creek carbonate-hosted REE–F–Ba deposit, British Columbia, Canada: constraints from Mg-Sr isotopes of dolomite, calcite, and fluorite. J Geochem Explor 240:107045. https://doi.org/10.1016/j.gexplo.2022.107045
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