Focus 1, 2023 - The graphite potential of Norway; Targets galore

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Håvard Gautneb står med en spade i en jordskråning.
Photo: Jan Egil Wanvik (NGU). Trenching at the Møkland graphite prospect.

The first NGU Focus sheet of 2023 covers the high graphite potential of Norway and is written by Håvard Gautneb.

Graphite in Norway

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Map of graphite provinces in Norway
(Fig. 1). Photo: NGU.

Norway has been a graphite producer for almost 100 years. Historically, graphite has been produced from three mines of which one, Skaland Graphite, is the only current producer. The Norwegian graphite deposits are all of flake graphite type and are all situated in Proterozoic rocks of upper amphibolite or granulite facies metamorphic grade.

Most of the deposits occur in three main provinces. Most of these areas are covered with new high-resolution Electromagnetic, Magnetic and Radiometric helicopter geophysical surveys. Apart from the mine in production very few of the Norwegian graphite deposits have been drilled or have any approved reserve calculation. Skaland graphite mine produces from the worlds richest flake graphite deposit, with an average grade of 31% graphitic carbon.

Graphite provinces

There are four known graphite provinces in Norway:

  • The island of Senja.
  • The Lofoten-Vesterålen islands.
  • Holandsfjorden area.
  • The Bamble area in southern Norway (Fig.1).

The Trælen deposit contains 1.8 Mt of proven reserves with a grade of 31% graphitic carbon. With the present annual production the mine has reserves for at least 50 years. The most extensive geophysical anomalies are associated with the Bukkemoen and Vardfjellet prospects with lengths of 2000 meters.

The island of Senja

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Airborne map of Senja.
(Fig. 2) Airborne (helicopter) EM map with the biggest new discoveries shown (red
arrow), old occurrences (black circle) on the island of Senja.

There are 14 occurrences and the active mine Trælen. (see Fig 2).

The Trælen deposit contains 1.8 Mt of proven reserves with a grade of 31% graphitic carbon. With the present annual production the mine has reserves for at least 50 years.

The most extensive geophysical anomalies are associated with the Bukkemoen and Vardfjellet prospects with lengths of 2000 meters.

Lofoten-Vesterålen

This archipelago has 26 different graphite occurrences and prospects, many of them on the island of Langøya. The Jennestad graphite mine was in operation from 1898-1914 and again from 1948 to 1962.

From 1990 to 1994 and from 2012 to the present, NGU investigated a number of known graphite prospects and new geophysical anomalies associated with graphite occurrences. A number of new prospects have been discovered and new information about ore grades is available.

Holandsfjorden

The Rendalsvik graphite mine in the Holandsfjord area was in operation from 1932-1947. New exploration in 1980 included a drilling programme of 660 meters which revealed a 30 meter wide, 300 meter long graphite orebody with an average graphite content of 9.5%.

Geological setting of the graphite deposits

All Norwegian graphite deposits occur in similar geological settings. The graphite ore typically occur associated with carbonates, intermediate and mafic gneisses and sometimes banded iron formations.

The graphite-bearing rocks are always folded and deformed in a complex manner involving polyphase folding, deformation and metamorphism up to granulite or high amphibolite facies. This rock association makes it most probable that the graphite-bearing rocks were initially part of a supracrustal rock association that comprised organic-rich sediments together with arenitic sandstones and intermediate to basic volcanic rocks.

On Senja and in Lofoten-Vesterålen the age of this supracrustal sucession is believed to be about 2 billion years.

The minerolgy of the graphite bearing rocks

The graphite-bearing rocks are quartz-feldspar rocks that can contain up to about 40% graphite, but a typical range is 5-25% (see Table 1).

The silicate minerals are typically (in descending order): Quartz, orthoclase, plagioclase, biotite, ortho-, and clinopyroxene.

Sulphides are in general minor phases. In situ in the rock, the graphite crystals occur as irregularly shaped grains with a typical grain size from 0.1 to 1.5 mm.

Deposit nameProvidenceLength (m)Width (m)% GCStatus
BukkemoenSenja20003005Deposit
HestenSenja1600506Deposit
VardfjelletSenja17005010Deposit
TrælenSenja40010031Active mine
GrunnvågSenja800168Deposit
FrøskelandVesterålen600507Prospect
SkogsøyaVesterålen 120010022Prospect
SvinøyaVesterålen 200623Prospect
SminesVesterålen 2000508Deposit
KvernfjorddalenVesterålen 40002015Prospect
Lille HornvannVesterålen 3005014Prospect
Hornvann/GrævaVesterålen 1002025Abandoned mine
GoliaVesterålen 2002018Abandoned mine
MøklandVesterålen 20005016Deposit
MorfjordVesterålen 3003015Abandoned mine
KovenVesterålen 8005013Abandoned mine
NordværnesHolandsfjord500505Abandoned mine
RendalsvikHolandsfjord 3003013Abandoned mine
DobbeBamble5002003Prospect
SundebruBamble 6002001,5Prospect
BjørnheiBamble 50418Prospect

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