More about the mineral deposit i Fen
Flyfoto over Fensfeltet med markering av bergart med sjeldne jordarter.
The dashed line shows the entire Fen Complex (5 km2), while the blue area shows the rare earth belt (1.5 km2). The blue field is the rock rauhaugite (Fe-dolomite-carbonatite) Photo: Sven Dahlgren.

The deposit of rare earth elements (REE) in the Fen Complex

How large is the deposit of REE in The Fen Complex? 

Author: Tor Espen Simonsen

Published: 14 Nov, 2023

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Updated: 28 Dec, 2023

In order to gain a better understanding of the Fen Complex's deposit of REE, it may be relevant to take a closer look at these factors:

  • The amount of rare earths in the bedrock
  • The grade or concentration of rare earths in the ore* (gehalt)
  • Rocks and minerals that contain the rare earths
  • The content of the various rare earth elements

In addition, it is important to take a closer look at what kind of tailings* and by-products mining can lead to. 

Read the short version of this text

  • The deposit of rare earths in the Fen Complex is significant, with an estimated volume of between 30 and 50 million tonnes (TREO*)
  • The grade of rare earths in the ore averages 1-2 percent, which is considered good.
  • Rare earths in Fen are primarily bound in the rock rauhaugite (Fe-dolomite-carbonatite).
  • The final picture of how the metals are distributed in the complex is still being explored. Extensive mapping remains before it can be determined whether the deposit is economically viable.
Read more:
Bildet viser kjerneprøver fra Fensfeltet.

The deposit measured in million tonnes

The Fen Complex is described as a very large deposit in a global context, and is probably by far the largest in Europe. A conservative estimate suggests that the Fens field contains between 30 and 50 million tonnes of rare earths (TREO*). In comparison, LKAB* has reported that the Per Geijer field at Kiruna may contain 1.32 million tonnes of TREO. 

According to the USGS , the total production of rare earths in the world was 300,000 tonnes in 2022. 

Grafisk fremstilling av forekomsten.
Within the area with the rock type rauhaugitt (FDC*) is believed to be a belt with a higher content of rare earths. This "belt" is marked in green on the map and is approximately 0.7 km2 on the surface. Photo: Sven Dahlgren.

Grade and concentration in the ore

Although the grade (gehalten) of REE in the Fen Complex is described as good, it may be somewhat lower than in some other known deposits in the world, such as Bayan Obo in China and Mountain Pass in the United States. It is believed that the average grade of rare earths in Fen is between 1 and 2 percent, with several richer zones at 3 to 5 percent. In the map above, the green-marked 'belt' is assumed to have the highest concentration of REE.

It can be challenging to grasp the significance of these percentages, and an grade of 1 or 2 percent may appear low. It is often helpful to consider such figures in relation to other well-known mineral projects:

  • The average concentration (gehalt) of niobium in Søve mines was slightly above 0.3 percent during the mining operations in the 1950s and 1960s   
  • In the Swedish Per Geijer field, a concentration of approximately 0.18 percent is estimated for rare earth elements.  
  • The copper deposit at Nussir in Finnmark, which has been granted an operating license by the state, has a copper concentration ranging from 1 to 1.1 percent
  • The titanium deposit at Førdefjorden (Engebøfjellet), which also holds an operating license, has a concentration of 4 percent (rutile/titanium). 
Rauhaugitt med REE-mineraler.
The rock type rauhaugite (Fe-dolomite-carbonatite). We can see the REE-minerals as brown-red spots in the stone.
Bilde av bergartene rødberg og rauhaugitt.
Rauhaugitt (on the right) is currently being surveyed based on its rare earth content. Rødberget (on the left) was the starting point for the iron mines in Fen.

Rock types and minerals

On Fen, it is the volcanic rock rauhaugite (Fe-dolomite-carbonatite) that is of interest.

In the rauhaugite, the rare earths are bound in phosphate (monazite) and fluorocarbonates (bastnäsite). These are the same minerals that rare earths are traditionally mined from elsewhere in the world.  For example in the USA and China. 

Although the concentration on Fen is «only» 1 to 2 percent on average, the rare earths appear in clusters or lumps. This can be favorable for extraction and separation.  

In the red rock, that dominates the old iron mines on Fen, there are also rare earths, but here they appear much finer grained and are therefore difficult to extract. At the same time, the content of radioactive thorium is higher in the red rock. 

The ratio between the various REE metals in the Fen Complex deposit

Another factor of interest in understanding the deposit in Fen relates to the distribution of the 17 rare earth species. Market prices vary significantly from one element to another, with the 'magnetic' metals like dysprosium and neodymium having the highest value.

Given that Fen shares important similarities with active deposits in the USA, China, and Australia, we can anticipate a similar proportion of key metals in Fen. This aligns with reports from researchers and licensees (companies) in the Fen area. Thus far, the consensus has been that the Fen Complex contains a 'healthy' amount of the most valuable raw materials

A final picture of how the various metals are distributed in the area of Fen will only come when the licensees have documented their deposits in more detail. 

Tailings and by-products

The mineral deposits of rare earth elements constitute only a small percentage of the ore. This implies that large volumes of tailings and waste rock must be managed once the valuable minerals have been extracted. 

This will likely involve the implementation of three parallel techniques: 

1) development of by-products

2) backfilling of tailings in the mine 

3) on-land disposal 

The rock type that contains rare earth minerals is often referred to as rauhaugite (re-dolomite-carbonatite). It primarily consists of carbonates (80 to 90 percent). NGU states that carbonate minerals, such as limestone and dolomite, are "Norway's most important industrial mineral group". Carbonate minerals are utilized in various industries, including the paper industry, cement production, and environmental applications such as acid neutralization. There is a potential opportunity to produce marketable by-products from the surplus materials at Fen.  

By-products can reduce the need for on-land disposal and enhance the financial viability of a mine. However, these by-products must meet cleanliness standards, and there will be a requirement to separate out radioactive thorium. Achieving this will be one of several critical success factors for mining in the Fen Complex.