REEX.no

In transition to clean energy, critical minerals bring new challenges

- IEA Publications

Rare Earth Elements 

Rare earth elements (REEs) comprise a group of 15 elements known as the lanthanides in the periodic table. Scandium and yttrium are commonly included due to their similar chemical properties and their occurrence in the same types of mineral deposits.


REEs are typically classified into light rare earth elements (LREEs)and heavy rare earth elements (HREEs). This classification reflects differences in atomic structure, geochemical behaviour, abundance, and industrial relevance. Light rare earth elements are generally more common in the Earth’s crust, whereas heavy rare earth elements are less abundant and often more challenging to source.


Rare earth elements play a critical role in a wide range of modern technologies. They are essential components in consumer electronics such as smartphones, displays, audio devices, and optical systems. High-performance rare earth magnets are key to wind turbines, electric and hybrid vehicles, and energy-efficient motors. REEs are also widely used in industrial catalysts, rechargeable batteries, and defence and guidance systems.

Due to their importance in clean energy technologies and advanced industrial applications, rare earth elements are increasingly recognised as strategically important raw materials.



The Fen carbonatite complex, a peralkaline-carbonatitic ring complex is situated near lake Norsjø in the Nome municipality in Telemark county, southeast Norway.
It consists of a circular 5 km2 core with various carbonatites and alkaline igneous rocks (mainly of the melteigite-ijolite-urtite series), intruded 583 +/- 10 Ma ago into Mesoproterozoic granitic Telemark Gneiss (ca. 1105 Ma old).

The intrusion was followed by intense faulting and brecciation, producing several phases through metasomatic alteration and fenitization of the country rock (Brøgger 1921, Sæther 1957, Andersen 1989,Verschure & Maijer 2005).

The original minerals of the gneiss, quartz, biotite and amphibole (hornblende), were altered or replaced by aegirine-augite and sodium amphiboles. Microcline and oligoclase were also replaced by mesoperthite and chessboard albite (Verschure & Maijer 2005).

A fenite aurole surrounds the western and southern parts of the complex, as well as metasomatic alteration of the fenite at the contact with the carbonatite (Kresten & Morogan 1986, Andersen 1989).


Source: Mindat.org

Pre-Feasibility and Feasibility

Three companies have exploration rights at the Fen Complex.


REE Exploration has been given
five substantial areas situated around the existing two search-companies.

Assessing Rare Earth opportunities

REE Exploration have the exclusive right to explore and assess FENSBUKTA 1-5 and have conversations with several geologists in relation to exploration areas.


We have also opened dialogue with several investors and possible co-owners. Exploration drilling program is assumed to start Q1 2023.