REE and Y Mineralogy of the Krudum Granite Body (Saxothuringian Zone)
Author:
Publisher
MDPI AG
Subject
Geology,Geotechnical Engineering and Engineering Geology
Link
http://www.mdpi.com/2075-163X/8/7/287/pdf
Reference54 articles.
1. Residence of REE, Y, Th and U in Granites and Crustal Protoliths; Implications for the Chemistry of Crustal Melts
2. Genesis and stability of accessory phosphates in silicic magmatic rocks: a Western Carpathian case study
3. Chemical composition of radioactive accessory minerals: implications for the evolution, alteration, age, and uranium fertility of the Fichtelgebirge granites (NE Bavaria, Germany)
4. Origin of monazite–xenotime–zircon–fluorapatite assemblages in the peraluminous Melechov granite massif, Czech Republic
5. Understanding geologic processes with xenotime: Composition, chronology, and a protocol for electron probe microanalysis
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3. Solubility of Monazite–Cheralite and Xenotime in Granitic Melts, and Experimental Evidence of Liquid–Liquid Immiscibility in Concentrating REE;Journal of Petrology;2021-03-08
4. Compositional Variability of Monazite–Cheralite–Huttonite Solid Solutions, Xenotime, and Uraninite in Geochemically Distinct Granites with Special Emphasis to the Strongly Fractionated Peraluminous Li–F–P-Rich Podlesí Granite System (Erzgebirge/Krušné Hory Mts., Central Europe);Minerals;2021-01-27
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