Rare Earth Elements

Often abbreviated as “REE”, these 16 elements include (preceded by their atomic numbers): 21 scandium (Sc), 39 Yttrium (Y) and the 14 elements that comprise the lanthanides excluding 61 Promethium, an extremely rare and radioactive element. These elements show closely related geochemical behaviors associated with their filled 4f atomic orbital. REEs are used to infer petrological mechanisms that have affected a rock due to preferential fractionation of some REEs relative to others. REEs are also useful for dating rocks, as some their radioactive isotopes display long half-lives.

  • LREE (light rare-earth elements) include these 8 elements (preceded by their atomic numbers): 57 lanthanum (La), 58 cerium (Ce), 59 praseodymium (Pr), 60 neodymium (Nd), 61 promethium (Pm), 62 samarium (Sm), 63 europium (Eu), 64 gadolinium (Gd). They are grouped together based on their increasing unpaired electrons.
  • Although Scandium is the lightest of the rare earths, it is not classified as a LREE or HREE due to its different chemical and physical properties and is considered in a class by itself.1
  • HREE (heavy rare-earth elements) include these 8 elements (preceded by their atomic numbers): 65 terbium (Tb), 66 dysprosium (Dy), 67 holmium (Ho), 68 erbium (Er), 69 thulium (Tm), 70 ytterbium (Yb), 71 lutetium (Lu) and 39 Yttrium (Y). They are grouped together based on their paired electrons.

As related to meteorites, REE patterns refer to the abundances of rare-earth elements relative to those in chondritic meteorites.

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