Regolith-hosted rare-earth elements: The phyllosilicate connection

Articles in the same Issue

1. Highlights and Breakthroughs
2. Regolith-hosted rare-earth elements: The phyllosilicate connection
3. MSA Centennial Review Paper
4. Heirs of the revolution: X-ray diffraction and the birth of the Mineralogical Society of America
5. Deep Earth carbon reactions through time and space
6. Magmatic carbon outgassing and uptake of CO₂ by alkaline waters
7. New insights into the evolution of Mississippi Valley-Type hydrothermal system: A case study of the Wusihe Pb-Zn deposit, South China, using quartz in-situ trace elements and sulfides in situ S-Pb isotopes
8. Celestine discovered in Hawaiian basalts
9. Microstructural controls on the chemical heterogeneity of cassiterite revealed by cathodoluminescence and elemental X-ray mapping
10. Hornblende as a tool for assessing mineral-melt equilibrium and recognition of crystal accumulation
11. The role of clay minerals in formation of the regolith-hosted heavy rare earth element deposits
12. The tetrahedrite group: Nomenclature and classification
13. Caseyite, a new mineral containing a variant of the flat-Al₁₃ polyoxometalate cation
14. Incorporation of Mg in phase Egg, AlSiO₃OH: Toward a new polymorph of phase H, MgSiH₂O₄, a carrier of water in the deep mantle
15. Imaging trace-element zoning in pyroxenes using synchrotron XRF mapping with the Maia detector array: Benefit of low-incident energy
16. Discussion
17. “Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of diamond formed by gas phase condensation or chemical vapor deposition—Discussion
18. Reply
19. On “Kamchatite” diamond aggregate from northern Kamchatka, Russia: New find of CVD-formed diamond in nature—Reply to K.D. Litasov, T.B. Bekker, and H. Kagi
20. Memorial of Enver Murad 1941–2019
21. Errata