Below is a description of REEs as they will be used on this website:*Table data from Rudnick & Gao (2003) | Rare earth oxides pictured at right
RARE EARTH OXIDE (REO)REO is the mathematical sum of La-Lu plus Y as their common oxides. Some call this total REO, TREO, TREO + Y, or YREO. Note, there is no such thing as REO in a geological environment. The REE-bearing minerals contain these elements as phosphates, carbonates, silicates, and others, with the term REO used for convenience. It originates from the early nomenclature referring to these elements as earths or oxides. The original gravimetric assay procedures provided results in REO % units, and also contained Th in the results when applicable. REO is produced only under laboratory or production conditions. Further, the individual REEs are often classified into subgroups:
- Light Rare Earth Elements (LREE) – La, Ce, Pr, Nd
- Mid Rare Earth Elements (MREE) – Sm, Eu, Gd
- Heavy Rare Earth Elements (HREE) – Tb, Dy, Ho, Er, Tm, Yb, Lu, Y
- When rare earths are referenced as only LREE or HREE, it is very important to understand which elements are being considered as LREE or HREE. These definitions have shifted over the past decade, with junior mining companies creating their own new set of definitions.
- Due to nuclear stability issues, the even atomic numbered REEs are more abundant than the nearby odd atomic number REE elements. This is why Ce is found in greater concentration than La, Nd greater than Pr, Sm greater than Eu, and Dy greater than Tb, etc.
- Pm is radioactively unstable, and at earth’s timescale has long ago decayed away to zero concentration. It is found in the appropriate nuclear reactions.
- Scandium (Sc) is often included with the REEs, but it is rarely found in REE deposits in appreciable amounts, and the market for Sc is distinctly different.