annex 1: greenland mineral deposit descriptions
TRANSCRIPT
Annex 1: Greenland mineral deposit descriptions
TABLE OF CONTENTS
CHROMIUM ........................................................................................................................... 3
COPPER ................................................................................................................................. 5
GRAPHITE .............................................................................................................................. 8
IRON .................................................................................................................................... 10
NIOBIUM AND TANTALUM .................................................................................................. 13
PGE ..................................................................................................................................... 15
REES -WITH FOCUS ON ND/DY ........................................................................................... 18
TUNGSTEN ........................................................................................................................... 21
ZINC .................................................................................................................................... 23
CHROMIUM
- Where in Greenland is chromium found and
where is the potential 1. In Southwest Greenland about hundred kilometres south of Nuuk, the
Fiskenæsset stratiform anorthosite complex occurs, with a combined strike
length of 200 km. The complex stretches from the coast to the edge of the
Inland Ice and is likely to continue under the Ice Cap. The anorthosite
complex has been metamorphosed in amphibolite facies and locally up to
granulite facies. The complex has furthermore suffered several phases of deformation, whereby the complex
has been broken up in sections ranging from
kilometres down to a few tens of metres in length.
Chromium occurs in the mineral chromite, which
is the dominating mineral in chromitites. Other
minerals in chromitites are hornblende and
plagioclase locally pyroxenes. Sulphides are rare
in chromitites. Chromitite bands occur in nearly
all stratigraphic units of the anorthosite complex.
Most commonly chromitite bands are found in
anorthosite and gabbro anorthosite, but chromitite
is also found in several ultramafic units. The
width of the chromitites ranges from centimetres
up to a few metres. In fold closures up to 20
metre thick chromitite bands are seen.
Composition of the chromite concentrates from
168 analysis varies considerably: Cr2O3: 27-35%;
FeO (total iron): 33-42%; Cr/Fe ratio: 0.60-0.93.
The general low Cr/Fe ratio shows that the
chromitite is not metallurgical ore. Rutile (TiO2)
occurs frequently as inclusions in chromite
amounting up to 0.35%. If mining of chromitite
takes place, rutile may be a valuable by-product
(Ghisler 1976).
2. At Ujaragssuit Nunât some 150 km northeast of Nuuk a small body of ultramafic rocks occur embedded in
gneisses. The ultramafic intrusion displays a complete magmatic evolution with seven cycles from dunite
through harzburgite to gabbro anorthosite. Chromitite layers up to ten centimetres thick each and metre thick
chromitite pods are seen. The presently exposed width of the intrusion is ~45 metres and length is ~150 m.
Chromite makes up 90 vol. % of the chromitite pods and less in the chromitite layers. The chemical
composition of chromite gave the following ranges: Cr2O3: 22-49%, FeO (total iron): 24-51%. Cr/Fe ratios
and range was not determined (Appel et al. 2002).
Greenland potential
3. The Seqi Olivine deposit which is located around 100 km north of Nuuk in southern West Greenland is a
fairly large dunite body (around 100 Mt) that has been exploited for olivine from 2005-2009. The deposit has
earlier been explored for chromite by the Cryolite
Company in the 1960’ies. However, the company
closed down decades ago and the reports describing
their findings have since been lost. The deposit thus
might have an undiscovered potential for Chromium.
- Known resources and reserves of
chromium in Greenland The chromium potential of the Fiskenæsset
anorthosite complex was investigated in some detail in
the 1970 to 1980’ies by the Canadian junior company Platinomino. No drilling was undertaken.
On the island of Qeqertarssuatsiaq a fairly continuous
chromitite band with width ranging from 1 to 7 metres
can be traced for ~1400 metres. The estimated tonnage
of this occurrence is of 2.5 Mt of chrome ore. For the
whole anorthosite complex an estimated 100 Mt of
chromium ore may be found.
The chromium potential of the chromitite banded intrusion northeast of Nuuk is, from an industrial purpose,
slightly more attractive than the chromite in the Fiskenæsset anorthosite complex. However, size of the
intrusive body is much smaller. The intrusive body was heavily deformed so there are likely extensions of
the intrusions in the general area, but they have not been found yet.
- Overview and status of projects exploring for chromium Only very limited exploration has been carried out for chromium in Greenland during the last thirty years.
While the world market for chromium seems to be well supplied, the exploration and the development of
some of the known chromite resources in Greenland might be triggered and led by their interesting PGE
contents.
- References Appel, C. C., Appel, P.W.U. & Rollinson, H.R., 2002: Complex chromite textures reveal the history of an
early Archaean layered ultramafic body in West Greenland. Mineralogical Magazine Dec. 202: vol.
66(6); p. 1029-1041.
Ghisler, M., 1976: The geology, mineralogy and geochemistry of the pre-orogenic Archaean stratiform
chromite deposits at Fiskenaesset, West-Greenland. In: Borthcert, H. (ed) Minograph Series on
Mineral Deposits, Borntraeger 126 pp.
Layered Archaean anorthosite with layers of chromitite. from the Fiskenæsset anorthosite complex
COPPER
- Where in Greenland is copper found and where is
the potential Although underexplored, many parts of Greenland could hold a good potential
for undiscovered sediment-hosted copper deposits. Sediment-hosted copper
deposits account for c. 23% of the world’s copper production and known reserves. They are also important sources of silver and cobalt, and some deposits are also produce other
metals such as lead, zinc, uranium, gold and platinum-group metals. Sediment-hosted copper are formed in
basins that contain large sedimentary formations of marine or large-scale lacustrine (lake) environments. In
Greenland, 40% of the ice-free landmass is made up of such environments and several smaller occurrences
of copper are known. However, the larger ones remain to be found.
Especially the sub-type, ‘Reduced-facies Cu’ deposit type, of sediment-hosted copper is important as they
characterized by good grades of 1–5% Cu and tonnages between 2.5 to above 450 million tons. This type of
deposit is sometimes also referred to as the Kupferschiefer-deposit after the type examples within a large
sedimentary basin in Poland; a basin that formerly were interlinked with similar basins in East Greenland
were similar, but smaller, copper occurrences also are known. Also the important copper deposits in DR
Congo are of a similar deposit type. Two other sediment-hosted copper sub-types, the so-called ‘Redbed Copper’ and ‘Revett Copper’ are found in Greenland; however, these constitute normally lower grades and lower tonnages.
The other main source of copper world-wide is ‘Porphyry-type deposits’ which constitute two-third of the
world’s copper. However, the potential for this type of deposit is thought to be smaller in Greenland as the typical geological environment of this type of deposit is not
present and as the crustal-exposure level in Greenland is too
deep compared to areas elsewhere in the world that contain
the major copper porphyry-deposits. Copper is also produced
as by-products from igneous nickel-deposits.
- Known resources and reserves of
copper in Greenland Very limited exploration for sediment-hosted copper
mineralisation has been carried out in Greenland. However,
the activity that have been carried out have, mostly based on
traditional surface-prospecting on exposed rock, successfully
identified several smaller copper occurrences throughout
many of the sedimentary basins in Greenland. Only a few of
these have been investigated in detail to a level which allow
for a geological estimate of overall tonnage and grade and
none of these, are of economically viable.
Distribution of tracts with sedimentary successions that are regarded as having potential for sediment-hosted copper deposits in Greenland. From Stensgaard et al. 2011.
Greenland potential
A first estimate of undiscovered resources in Greenland is included in the table below. The undiscovered
copper resource estimates are derived from a statistical simulation which used globally tonnage/grade models
for known deposits worldwide and bids on number of undiscovered sediment-hosted copper deposits within
different sedimentary basins in Greenland. The bids are from the 2009 workshop on the “Assessment of the sediment-hosted copper potential in Greenland” (Stensgaard et al. 2011). The exact estimates should be used
with precautions and will, besides always being a statistical derived estimate, be a reflection of confidence
and how much is known and how many data that is available from an area.
Estimate of undiscovered copper resources (metric tons of Cu metal)
Areas Reduced Cu Revett Cu Redbed Cu Source
Permian, Jameson Land Basin, East Greenland 240,000 t 568,000 t none Stensgaard et al. 2011
Triassic, Jameson Land Basin, East Greenland 1,130,000 t none 38,000 t Stensgaard et al. 2011
Neoproterozoic, Eleonore Bay Basin, East
Greenland
1,540,000 t none none Stensgaard et al. 2011
Neoproterozoic, Thule Basin, Norht-West
Greenland
160,300 t none none Stensgaard et al. 2011
- Overview and status of projects exploring for copper In terms of copper exploration in Greenland a couple of projects are presently carried out. The junior
exploration company Avannaa Resources Ltd. is in partnership with Angle American exploring for
sediment-hosted copper in central East
Greenland. Another company, China
Nordic Mining Company Ltd. is also
carrying out exploration for copper in
central East Greenland. China Nordic
Mining Company Ltd. is backed by the
Jiangxi Copper, which is China’s biggest producer of the metal.
In the context of igneous nickel-deposits
and copper as by-products in such
deposits, the Maniitsoq nickel-copper-
cobalt-PGM project owned by North
American Nickel should be mentioned.
- Recommendations Most of the exploration that has been carried out for copper in Greenland has been based on traditional
surface prospecting assisted by geochemical prospecting. Only very seldom have surface sampling, even
though it has resulted in good grades and continuity resulted, been followed up e.g. geophysical methods or
drilling that would widen up the search-space and make it possible to look beyond the surface exposure.
Geophysical surveys include aeromagnetic, gravimetric and hyperspectral surveys covering the most
prospective sedimentary basins is recommended, as well as more detailed survey programs around some of
the known surface-identified copper occurrences. These surveys can assist in identifying main structures
controlling the distribution of mineralisation, which should subsequently be followed-up with field
reconnaissance expeditions. These would facilitate and stimulate mineral exploration and possibly lead to
new discoveries. Considering the high exploration costs, matched-grants to exploration and drilling
programs, to facilitate discoveries, could also be considered.
A more complete evaluation of the potential sedimentary-basin prospective for copper would greatly benefit
from funding dedicated to deepening the cooperation with e.g. researchers and copper producing companies
Malachite-stained outcrop of quartzitic sandstone from the Brogetdal copper occurrence in Strindberg Land, North-East Greenland. From Stensgaard et al. 2011.
in Europa, e.g. with Poland, as the basin that holds some of the larger copper deposits in Poland continues to
East Greenland.
Field work studies, both for research and exploration, require the availability of key logistical platforms in
remote areas, particularly in East, North and North-West Greenland. Likewise, research on effective and
mobile mining infrastructure / energy supplies in high Arctic areas are strongly recommended.
- References Geology and Ore, No 18: Sediment-hosted copper in Greenland, Geological Survey of Denmark and
Greenland, 12 pp.
Stensgaard, B.M., Kalvig, P. & Stendal, H. 2011: Quantitative mineral resource assessment: Sedimentary-
hosted copper in Greenland - Reporting the copper assessment workshop, GEUS, Copenhagen,
March 2009. Danmarks og Grønlands Geologiske Undersøgelse Rapport 2011/104, 170 pp + 1 CD-
ROM.
International Copper Study Group, ICSG. www.icsg.org
USGS Minerals Information, Copper, Statistics and Information,
http://minerals.usgs.gov/minerals/pubs/commodity//copper/
GRAPHITE
- Where in Greenland is graphite found and where
is the potential The reworked, deformed and metamorphosed Palaeoproterozoic orogeny and
the Palaeoproterozoic mobile belts of Greenland have relatively high abundance of graphitic material, mostly
hosted in supracrustal rocks. In many cases it seems that the greatest abundance of graphite is located in or
near large scale faults or shear zones.
- Known resources and reserves of graphite in Greenland A compilation of the distribution of known occurrences with resource estimates in Greenland is included in
the table below.
Resources in known deposits
Deposits: Ton/grade Type Source:
Amitsoq 250,000 t @ 20-24% Graphite Geological resource (Non complient)
Bondam 1992; Mosher 1995
Akuliaruseq (Eqalussuit) 5.3 Mt @ 9.5% Graphite
Geological resource (Non complient)
Kalvig 1992
1.37 Mt @ 14.1% Graphite Mineable resource (Non complient)
Bondam 1992
Kangikajik 500,000 t @ ? Geological resource (Non-complient)
Kalvig 1992, 1994
Grænseland 10,000 t Geological resource (Non complient)
- Overview and status of projects exploring for graphite Graphite occurrences are known from many localities in Greenland as indicated on the map; however most
of them are too small to be commercially exploitable or needs more exploration activities to develop the
projects.
Akuliaruseq is the only graphite occurrence that is
currently being investigated by an exploration company.
The deposit is located in central West Greenland around
140 kilometers from the International airport at
Kangerlussuaq. Knowledge of the Akuliaruseq deposit
goes back as far 1912-1916 where sporadic mining took
place. No further work was done until the 1980s.
From 1982 to 1986 the Danish Cryolite Company
carried out exploration work to test the extent of the
graphite layers including 5,700 m drilling. In 1990 and
2000 the quality of the deposit was tested by Nunaoil
and NunaMinerals.
The current license-holder of the Akuliaruseq deposit,
21st North are planning 5,000 m of drilling, bulk
sampling of both low-grade and high-grade material to
test the flake size distribution throughout the
mineralised sequence and beneficiation/test mining
Greenland potential
studies on bulk samples in order to indicate ash melting points, level of purification and recovery and
grade upgrade.
The graphite layer and old entrance at the Amitsoq graphite mine in South Greenland.
- Recommendations The discovery potential for graphite deposits with the Palaeoproterozoic parts of Greenland is moderate to
high and could benefit from high-resolution geophysical and remote sensing surveys. Recommended surveys
thus include aeromagnetic, gravimetry and hyperspectral surveys covering the tracts with potential indicated
on the map. These surveys can assist in identifying the large scale structures controlling the distribution of
mineralisation, which should subsequently be followed-up with field reconnaissance expeditions. These
would facilitate and stimulate mineral exploration and possibly lead to new discoveries.
- References 21st North Website: http://www.21stnorth.com/Projects.html
Bondam, J. 1992: Graphite occurrences in Greenland - A review. GGU Open File Series 92/6, 32 pp.
Kalvig, P. 1992: Geologiske undersøgelser af grafitforekomsten Kangikajak, Tasiilaq Kommune. Internal
report, Tasiilaq Kommune, 41 pp.
Kalvig, P. 1994: Industrial mineral occurrences in Greenland - a review. GGU Open File Series 94/4, 94 pp.
Mosher, G. 1995: Summary of mineral occurrences and mineral exploration potential of South Greenland
(Sheet 1 Geological map of Greenland). GGU Open File Series 95/3, 35 pp.
IRON
- Where in Greenland is iron found and where is
the potential The Greenland iron ore potential is mainly based on Archaean sedimentary
and chemical iron deposits (BIF) of the so-called Algoma type, which are
typical for Archaean greenstone belts formed in continental rifts or at
continental margins. BIF type occurrences deliver the majority of iron ore
and are amongst the world’s most important iron sources. However, notable occurrences related to Palaeoproterozoic magmatism have recently been
demonstrated to account for prominent iron ore
accumulations in Inglefield Land, in North Greenland, and
at Isortoq in the Gardar province in South Greenland.
The last decades renewed interest in exploration for iron
ore in Greenland reflects an increase in iron-ore prices,
driven by demand from emerging Asian economies. Most
exploration in Greenland has been focused on the known
and proven deposits like the Isua and Itilliarsuk BIF’s, but since 2011 the more remote and less-explored part of the
Melville Bay area in North-West Greenland has been
explored for BIF’s hosted by a sequence of
metamorphosed sedimentary and volcanic rocks that share
a common evolutionary history with the Mary River and
Prince Albert Groups of Baffin Island and mainland
Nunavut, Canada.
- Known resources and reserves of
iron in Greenland A compilation of the distribution of known indicated and
inferred iron resources in Greenland is included in the
table below.
Resources in known deposits
Deposits: Ton/grade Type Source: Isua 380 Mt @ 33 % Fe Indicated JORC resource London Mining 727 Mt @ 32 % Fe Inferred JORC resource London Mining
Isortoq 70 Mt @ 29.6% Fe, 10.9 % TiO2, 0.144 % V2O5
NI43-101 compliant inferred resource
West Melville Metals
Havik (Melville Bay) 67 Mt @ 31.4 % Fe JORC Inferred resource Red Rock Resources
- Overview and status of projects exploring for iron There are a fairly large amount of known iron occurrences in Greenland as indicated on the map, but most is
too small to be commercially exploitable or needs more exploration activities to develop the projects.
Greenland potential
In order to mature the Isortoq Iron project towards exploitation stage, West Melville Metals is planning to do
more infill drilling and metallurgy testing as well as conducting high–resolution airborne magnetic survey
covering the entire property. In addition
Environmental baseline studies and
meetings with the local communities will
be completed.
Red Rock Resources have identified
additional exploration targets of up to 200
Mt haematite and 1 Bt magnetite in the
Melville Bugt region and thus need to
conduct more drilling in the area. The
company is currently looking for potential
farm-in partners and has no plans for
exploration in 2014.
In terms of planned production, the most
advanced project is the Isua project, by
London Mining, which has just been
granted an exploitation license ultimo 2013. The mining operation will have an expected mine life of 15
years, with a production rate of 15 Mt/a from an open pit mining operation. London Mining needs an initial
capital investment of USD2.35 billion for the development of the project and is thus currently looking for
investors.
- Recommendations The technical demands of maintaining mining and export operations in the high Arctic necessitates a degree
of capital expenditure, however the scale of deposits that have been identified in recent years proves that
Arctic exploration is worth investment.
Most of the exploration that has been carried out for iron in Greenland has been based on traditional surface
prospecting assisted by geochemical prospecting and regional geophysical surveys. However, the fairly
recent discoveries of the Havik and Isortoq deposits by high-resolution aeromagnetic surveys suggest that
there is a large potential for undiscovered iron deposits in Greenland. Therefore, it is recommended to
conduct detailed aeromagnetic geophysical surveys in selected regions in Greenland that also includes,
gravimetric and hyperspectral surveys. This would facilitate and stimulate mineral exploration and possibly
lead to new discoveries as seen in Nunavut after the Government completed a regional detailed aeromagnetic
survey. Considering the high exploration costs, matched-grants to exploration and drilling programs, to
facilitate discoveries, could also be considered.
One of the main challenges facing burgeoning iron producers is the logistics of transporting ore to world iron
customers. Various iron projects have been identified worldwide with many currently stalled in development
due to delays caused by inadequate rail and port logistics. Governments are slow to react to changing
requirements and affected communities adopt a hostile approach, resisting and blocking expansion.
Therefore one of the keys to developing a successful iron ore project is ensuring that the project has a
pathway to market.
- References
London Mining Greenland A/S website: www.londonmining.com/
Red Rock Resources website: www.rrrplc.com/
Close-up of the BIF sequence at Pingorssuit, North-West Greenland.
Stendal, H. & Secher, K. 2011: Iron ore potential in Greenland. Geology and Ore No. 19, 12 pp.
Thomassen, B. 2008: The Thule Iron Province, North-West Greenland. A compilation of geological data. 2.
Revised edition. Danmarks og Grønlands Geologiske Rapport 2008/61. 28 pp. + CD-ROM
West Melville Metals website: www.westmelville.com/
NIOBIUM AND
TANTALUM
- Where in Greenland is niobium (Nb) and tantalum (Ta) found and
where is the potential Niobium and tantalum does not occur as native elements, but most frequently in Nb-Ta-oxides including
minerals like columbite, tantalite and pyrochlor. Nb-Ta deposits are normally hosted in three types of
deposits: Carbonatite-hosted deposits (Nb); alkaline to peralkaline granites and syenites (Nb, REE, Zr, Sn
and Ta) and in peraluminous pegmatites and granites (Ta, Nb, Sn, W, Zr, Ce and Ta).
In Greenland the Mid-Proterozoic Gardar Province of South Greenland has by far the highest potential for
Nb and Ta deposits, encompassing the Kvanefjeld and Kringlerne deposits of the Ilimaussaq Complex, and
the Motzfeldt Center of the Igaliko Complex, hosting evolved syenites and granites. A few of the known
carbonatite occurrences on the West coast of Greenland are enriched in Nb (and Ta).
- Known resources and reserves of Nb and Ta in Greenland A compilation of known Nb and Ta deposits in Greenland is included in the table below. The resource
estimates are derived from license holder websites.
Locality Type of resource
estimate
Tonnage
(Mt)
Grade (%
Nb2O3)
Grade (%
Ta2O3)
Licensee
Motzfeldt Altered
syenite
(Not JORC
complient) Scoping
>500 0.18 – 0.22 0.01 RAM Resources
Motzfeldt Peralkaline
sheet complex
(Not JORC
complient) Scoping
>80 0.4 -1.0 0.01 RAM Resources
Ilímaussaq Kringlerne JORC Indicated 4300 0.2 0.02 Tanbreez
Sarfartoq JORC Indicated 0.19 4.6 ? Hudson Resources
- Overview and status of projects exploring for Nb and Ta in Greenland The following projects that mainly explores for REE´s also contain Nb/Ta as by-project and could thus be a
future provider of these commodities.
The Kringlerne Project: The REE-deposit occurs in the eudialyte mineral of the kakortokite, constituting
the lower layered part of the Illimaussaq Complex, grading 0.6% TREO, 0.25% Nb2O3, and 0.025 Ta2O3.
The license holder Tanbreez Ltd. submitted exploitation license Nov. 2013, and anticipates start of operation
in 2016. The project intends to mine open pit near the fjord; the ore will be trucked to an adjacent process
plant, producing three products: (i) eudialyte concentrate; (ii) feldspar concentrate, and (iii) arfvedsonite
concentrate, which will be shipped for further processing and/or use outside Greenland. The planned annual
production is 500,000 ton, equivalent to a maximum of 1,250 ton Nb2O3, and 125 ton Ta2O3.
Greenland potential
Kvanefjeld REE-Project: The Kvanefjeld REE-U-
deposit also hosts Nb-carrying minerals, and thus
carries the potential to become a by-product Nb
producer; feasibility studies are on-going. However,
no production of neither Nb nor Ta is considered at
the moment.
Motzfeldt Sø Project: Australian company Ram
Resources Ltd. has acquired the Motzfeldt
polymetallic deposits. The Motzfeldt Centre
consists of a number of igneous intrusions of
peralkaline syentie and nepheline syenite covering.
In addition to the Nb and Ta, the Motzfeldt Sø
syenite holds significant amounts of REE at the
Aries Prospect mainly hosted by pyrochlore and
eudialyte. The mineralisation of REE and Nb-Ta are
only weakly correlated. Exploration is ongoing and
more work is required to define a JORC compliant
reserve/resource estimate.
The Sarfartoq Project: The central zone of the
complex surrounded by a series of ring-like dykes
containing numerous carbonate breccia veins.
Mineralisation of Nb and REE has been recorded from separate zones, where hydrothermal activities have
caused enrichment of Nb (and Ta). The license holder, Hudson Resources is undertaking scoping studies on
REE, U, and Nb-Ta.
- Conclusion The World’s primary reserves and resources of niobium and tantalum are estimated to be more than sufficient to meet global demand for many years ahead. This is why the interest in the new Nb/Ta-
exploration campaigns is rather modest and typically only occur in connection with REE deposits, where
Nb/Ta often is contained within the same minerals as the REEs.
- References Hudson Resources website: www.hudsonresources.ca
Ram Resources website: www.ramresources.com.au
Tanbreez website: www.tanbreez.com
Tukiainen. T. 1986: Pyrochlore in the Motzfeldt Centre of the Igaliko Nepheline Syenite Complex, South
Greenland, Final Report. Unpublished internal GGU report. 98 pp.
Tukiainen. T. 1988: Niobium-tantalum mineralisation in the Motzfeldt centre of the Igaliko nepheline
syenite complex, South Greenland. In: Boissonnas J, Omenetto P (eds) Mineral deposits within the European
community. Springer, Berlin, p. 230–246.
USGS 2013: Mineral Commodity Summaries 2013. US Geological Survey 2013, 198 pp.
PGEs
- Where in Greenland are PGE found and where
is the potential 1. The PGE-gold mineralisation in the Skaergaard intrusion, also referred
to as the Platinova Reef, is the most intensively studied and explored PGE
deposit in Greenland. The mineralisation defines its own class the
“Skaergaard-type” (Miller & Andersen, 2002). It is located at ~68 degrees N in East Greenland.
The mineralisation is concordant with the magmatic layering in the upper part of Middle Zone gabbros in the
Layered Series of the intrusion (Holwell & Keays, 2014) and comprises a lower main PGE “reef” followed by up to four additional PGE-rich levels of mineralisation. Only the central part of the intrusion show all five
levels significant PGE (>300ppb). The PGMs are totally dominated by the intermetallic alloy skaergaardite
(PdCu) with up-section increase in gold. The main gold resource is in the uppermost of developed PGE
levels and a level above. Au is dominantly hosted in intermetallic alloys such as tetra-auricupride (Au3Cu)
and auricupride (AuCu). At the margins of the intrusion only few meters separate the PGE and gold rich
levels of mineralisation, whereas in the centre of
the intrusion they are separated by >40m.
2. In Southwest Greenland about hundred
kilometres south of Nuuk, the Fiskenæsset
stratiform anorthosite complex occurs with a
combined strike length of 200 km. The complex
stretches from the coast to the edge of the Inland
Ice and is likely to continue under the Ice Cap.
The anorthosite complex has been
metamorphosed in amphibolite facies and locally
up to granulite facies. The complex has
furthermore suffered several phases of
deformation, whereby the complex has been
broken up in sections ranging from kilometres
down to a few tens of metres in length.
Chromitite layers are seen in several stratigraphic
levels in anorthosite and gabbro anorthosite.
Some of the chromitite layers contain sparse
sulphides. Many of the chromitites in the
anorthosites and gabbro anorthosites show
elevated PGE contents up to 600 ppb Pt, 300 ppb
Pd and 300 ppb Au (Appel et al. 2011).
The most promising PGE mineralisations so far found are in the coastal area in a 5 km long and up to 1 km
wide ultrabasic unit of the anorthosite complex. The zone was not broken up during deformation of the
Greenland potential
anorthosite complex. The mineralised rocks comprise olivine-rich peridotites, hornblende peridotites and
pyroxenites. Detailed mapping of the mineralised
zone has been carried out as well as channel
sampling along several profiles. The best results
obtained are found in the so-called Ghisler reef
which grades 690 ppb Pt, Pd and Au over 5
metres. Local higher grade parts contain 2 ppm
Pt, Pd and Au with 20 ppb Rh over 1 meter.
Ghisler reef displays an unusual geochemical
signature with near perfect correlation of Pt, Pd,
Au and Cu with Bi, thereby resembling the PGE
deposits in Sudbury (Canada), Great Dyke
(Zimbabwe) and the Monchegorsk intrusion on
Kola Peninsula (Russia) (Appel et al. 2011).
3. Lesser investigated occurrences with a potential includes:
a) The Norite Belt of the Maniitsoq region in West Greenland the (64 degrees N in West
Greenland, is presently understood as the result of meteoric impact and sulphide mineralisation
rich in nickel and Cu, as well as PGE, and compared to the Sudbury Ni-Cu-PGE district (www.
northamericannickel.com).
b) Palaeogene sulphide deposits in the feeder systems of the West Greenland Flood Basalt
Province (www.avannaa.com). The deposit type is expected to be similar to those of the
Noril´sk region (Russia).
c) Additional occurrences, mostly little investigated, are found in mafic intrusive bodies in the
Precambrian of West Greenland, e.g., the Amikoq mineralisation (www.nunaminerals.com),
and Palaeogene intrusions in East Greenland (Nielsen, 2002). A review of PGE potential in
Greenland can be found in Secher et al. (2007)
- Known resources and reserves of PGE in Greenland At Skaergaard, the geologic estimate suggests a >500 Mt resource with a total of ~36 million oz PGE and
~12 million oz. gold, classifying the deposit as a giant (Nielsen et al., 2005). The Pd/Pt is near 13 in the
deposit. No other PGE are present in economic concentrations. On the basis of cores drilled by the present
concessionaire, only, the sum of indicated and inferred resources is ~10 million oz. PGE and 6 million oz.
gold. Grades may reach ~5 g/t PGE and ~10 g/t gold, dependent on sample size (Watts, Griffis & McOuat,
1991)
- Overview and status of projects exploring for PGE The challenge in the Skaergaard mineralisation is the development of exploitation methods for the low grade
but large deposit type. The structure, mineralogy and continuity of the mineralisation is well documented. In
all other Paleogene occurrences in East Greenland the lack of exploration and the remoteness of many of
these constitute obvious constraints to their development. In addition, all other observed occurrences appear
to be discontinuous and related to contacts between intrusions and host rocks or between intrusive phases of
the intrusions. The potential for Noril´sk type mineralisations in the Palaeogene of West Greenland, appears
unquestioned at the present level of information. The potential related to the Ni-Cu-PGE occurrences in the
Norite Belt appears to increase with the accumulation of drill core data.
Channel sampling of mineralised layers in the Upper Zone, of the Skaergaard Intrusion, southern East Greenland.
As for many Palaeogene occurrences, the lack of focussed exploration is evident for anorthositic as well as
other mafic complexes in West Greenland, whose potential remains significant.
- References Appel, P. W. U., Dahl, O., Kalvig, P. & Polat, A. 2011: Discovery of new PGE mineralisations in the
Precambrian Fiskenaesset anorthosite complex, West Greenland. Danmarks og Grønlands
Geologiske Undersøgelse Rapport 2011/3 2nd edition 48 pp.
Holwell, D. & Keays, R.R. 2014: The formation of low-volume, high-tenor magmatic PGE-Au sulfide
mineralisation in closed systems: evidence from precious and base metal geochemistry of the
Platinova reef, Skaergaard Intrusion, East Greenland. Economic Geology, 109, p. 387-406.
Miller and Andersen, J.C.O. 2002: Attributes of Skaergaard-Type PGE Reefs. In Boudreau, A. (ed.).
Extended abstracts, 9th internat. Platinum Conf. p. 305-308.
Nielsen, T.F.D. 2002: Palaeogene intrusions and magmatic complexes in East Greenland, 66 to 75o N. GEUS
report 2002/113, 249 pp.
Secher, K., Appel, P. & Nielsen, T.F.D. 2007: The PGE potential in Greenland. Geology and Ore no. 8,
February 2007, 12 pp.
Watts, Griffis & McOuat 1991: 1990 Skaergaard project, Platinova/Corona concession, East Greenland.
Exploration report, 55 pp. and appendixes (in archive of the Geological Survey of Denmark and
Greenland, GRF no. 20848).
REEs -WITH FOCUS ON Nd/Dy
- Where in Greenland is REE found and where is
the potential Several REE-occurrences are known in Greenland; the largest deposits by
far are the igneous alkaline intrusions related to the Gardar Province in
South Greenland, hosting the deposits around Kvanefjeld, Kringlerne, and
Motzfeldt Sø; additionally four carbonatite related deposits are known
from the West coast, one alkaline intrusion and one fossil placer deposits,
both located in East Greenland.
- Known resources and reserves of REE in Greenland An overview of the resource figures for the most important Greenlandic REE-deposits is given in the table
below; additionally the potential co- and/or by-product grades are listed. Elevated radioactive mineralisation
are associated with most of the deposits; though the Kringlerne deposit is known to host only very little
uranium and thorium.
Locality Metallogenetic
type
Type of
resource
estimate
Exploration
status
Tonnage
(Mt)
Tonnage
TREO
(Mt)
Grade (%)
TREO
HREE
(%)
Grade Co-/by
products
Kvanefjeld Alkaline igneous JORC-
Indicated Feasibility 437 4.77 1.09 12
U: 274 ppm
Zn: 0.22%
F: n.a.
Sørensen Alkaline igneous JORC -
Inferred Feasibility 242 2.67 1.1 13
U: 304 ppm
Zn: 0.26%
F: n.a.
Zone 3 Alkaline igneous JORC –Inferred
Feasibility 95 1.11 1.16 12
U:300 ppm
Zn: n.a.
F: n.a.
Kringlerne Alkaline igneous JORC -
Inferred Feasibility 4,300 28 0.65 31
Zr3O8: 1.8%
Nb2O3: 0.2%
Motzfeldt Alkaline igneous n.a.-
Inferred Exploration 340 0.9 0.26 19
Ta2O3:120 ppm
Nb2O3:1850 ppm
ZrO2:4600 ppm
NIAQ Karrat Carbonatite
associated? n.a. Exploration 26 0.3 1 13 n.a.
Sarfartoq (ST1) Carbonatite
associated
NI 43-101
- Inferred Scoping 14.1 0.2 1.53 2 n.a.
Qeqertaasaq Carbonatite/Vein
associated n.a. Exploration 45 0.5 1 1 Nb2O3
Milne Land Fossil placer n.a. Exploration 5 0.1 1 13 2% ZrO2
- Overview and status of projects exploring for REE The Kvanefjeld Project encompasses the deposits Kvanefjeld, Sørensen, and Zone 3, of which the first is the
main target. The license holder Greenland Minerals and Energy Ltd (GME), expect to submit an application
for exploitation early 2015, enabling the company to commence production in 2018. The mining technique
will be by open pit, and the ore will be treated in an adjacent metallurgical plant, extracting the sphalerite by
flotation, and subsequently the steenstrupine concentrate will be fed into a hydrometallurgical leaching
circuit and uranium and REE are recovered by solvent extraction. GME has recently decided to locate the
hydrometallurgical leaching plant in Greenland and to undertake the REE-separation in China.
Greenland potential
GME estimates that neodymium and dysprosium will
contribute respectively c. 32% and 13% to the overall
value. Planned annual production: 10-20,000 ton
TREO, encompassing 1.200–2.400 ton Nd2O3 and
100–200 ton Dy2O3.
Kringlerne: The REE-deposit occurs in the lower
layered part of the Illimaussaq Complex. The license
holder Tanbreez applied for an exploitation license in
Nov. 2013, and expects to start operation in 2016. The
project intends to mine open pit near the fjord; the ore
will be trucked to an adjacent process plant, producing
three products: (i) eudialyte concentrate; (ii) feldspar
concentrate, and (iii) arfvedsonite concentrate, which
will be shipped for further processing and/or use
outside Greenland. Planned annual production: 3,250
ton TREO, encompassing c. 400 ton Nd2O3 and c. 90
ton Dy2O3.
Motzfeldt Sø: The Motzfeldt Centre consists of a
number of igneous intrusions of peralkaline syentie and
nepheline syenite covering. In addition to the REE, the
Motzfeldt Sø syenite holds significant amounts of Nb-
Ta at the Aries Prospect (estimated 500 Mt grading
120 ppm Ta; 130 Mt grading around 0.5% Nb2O5);
Nb-Ta and the REE are only weakly correlated.
Exploration is ongoing.
Sarfartoq: The central zone of the complex surrounded by a series of ring-like dykes containing numerous
carbonate breccia veins. Mineralisation of Nb and REE has been recorded from separate zones.
Qeqertaasaq: The license holder, NunaMinerals undertakes
simultaneous exploration and metallurgical tests on a new site, in
which promising surface samples yielding up to 13.2% TREO. The
mineralisation is LREE-dominated. NunaMinerals have ultimo
2013 signed a joint exploration agreement with Korea Resources
Corporation (”KORES”) in order to advance the project.
NIAQ Karrat: License holder, Avannaa Resources. Initial drilling
was undertaken in 2010. The average drill intersections yielded
about 1% TREO, and the HREO-ratio is c. 13%; initial
metallurgical testing on a bulk sample graded 1.1% TREO, Nd
0.2% and Dy 0.02%.
- Recommendations The planned annual production from the two most advance REE-projects in Greenland, Kvanefjeld and
Kringlerne, is in the range of 13,000-23,000 tons TREO. Öko-Institut (2011) estimates the 2014-supply for
neodymium and dysprosium to be about 33,000 and 2,000 tons/y respectively; if so the Greenlandic
Drilling at Kvanefjeld. Copyright GME.
production then may contribute to 5-8% of the global neodymium supply and 10-16% of the global
dysprosium supply.
The REE-deposits in Greenland contribute significantly to the global TREO-resource base, as well as the
anticipated production on particularly dysprosium carries a significant supply potential against the 2016
global demand.
The current global TREO resource base is estimated to be sufficient for 800 years of production based on a
200 K ton/y. This is contrast to the increasing undersupply of CREO, mainly due to the Chinese monopoly of
the REO-market. In order to erodate the Chinese monopoly on the REE-value chains, it is important to
support viable alternatives. Greenland offers two world-class REE deposits (Kvanefjeld and Kringlerne)
which theoretically have a strong market potential. Thus development of the South Greenland region in
terms of hydropower, local airport and harbour facilities would not only benefit the general development of
this region, but may as well make Greenlandic REE-operations more competitive.
- References
Naalakkersuisut 2012: Status for råstoffer. Presentation by Jørn Skov Nielsen, Departementet for Erhverv,
Råstoffer og Arbejdsmarked.
Roskill 2012: Rare Earths & Yttrium: Market Outlook to 2015. 527 pp., Fourteenth Edition, 2011. Roskill
Information Services Ltd., UK
Schüler, D., Buchert, M., Liu, R., Dittrich, S. & Merz C. 2011: Study on Rare Earth and Their Recycling.
Final Report for the Greens/EFA Group in the European Parliament, Öko-Institut, 162 pp.
Sørensen, L.L. & Kalvig, P. 2011: The rare earth element potential in Greenland. Geology & Ore No. 20, 12
pp.
Technology Metals Research 2014: TMR Advanced Rare-Earth Projects Index.
http://www.techmetalsresearch.com/metrics-indices/tmr-advanced-rare-earth-projects-index/
TUNGSTEN
- Where in Greenland is tungsten found and where is
the potential Economic tungsten (W) deposits are mainly of two types (vein and skarn)
related to granitic intrusions or medium to high-grade metamorphic rocks.
Numerous tungsten mineralisations are known from east and west Greenland, but they are especially
concentrated along a ~500 km belt in central East Greenland (see map below). Here outcropping tungsten
occurrences (occur as the mineral scheelite) are known from at least 12 areas with footprints varying from 1
to 20 km2 in size, and scheelite-bearing
boulders have been located in another two
areas.
It is possible to divide the scheelite-mineralised
areas in central East Greenland into three
groups on account of their geological setting.
The groups and their respective areas are as
follows:
Scheelite mineralisation in Upper
Proterozoic meta-sediments, often
spatially associated with Cale-donian or
older granitic intrusions.
Scheelite mineralisation in the Lower
Neoproterozoic sediments, up to 7 km
from outcropping Caledonian granites.
Scheelite mineralisation in fault zones in
Upper Neoproterozoic sediments without
spatial relation to granitic rocks. The areas
of this group comprise among others
North and South Margerie Dal on Ymer Ø.
- Known resources and reserves of tungsten in Greenland A compilation of the distribution of potential undiscovered and known tungsten resources in Greenland is
included in the table below. The potential undiscovered tungsten resource estimates are derived from a
workshop in 2013 on the “Assessment of the tungsten potential in Greenland” (Sørensen et al. 2014):
Undiscovered tungsten resources
(metric tons W metal) Resources in known deposits
Greenland potential
Areas Vein Skarn Source Deposits Tons/grade Type Source
Central east and
northeast
Greenland
179 267 Sørensen et al. (2014)
Ymer Ø – South
Margerie Dal
75,000 t @
2.5 % WO3
Scoping
study
Sørensen et al.
(2014)
Ymer Ø – North
Margerie Dal
42,000 t @
0.7 % WO3
Scoping
study
Sørensen et al.
(2014)
Northwest
Greenland 4.5 2.2
Sørensen et al. (2014)
South Greenland
43.2 4.8
Sørensen et al. (2014)
Summary of resource estimates for tungsten potential in Greenland and reported resources from known deposits.
- Overview and status of projects exploring for tungsten Current projects exploring for tungsten are few. NunaMinerals A/S holds a license on Ymer Ø exploring for
tungsten, antimony and gold. In May 2014, NunaMinerals A/S signed a Memorandum of Understanding with
the Canadian company, Northcore Resources Inc. to advance the development of the Ymer Ø project towards
exploitation.
- Recommendations Considering the limited exploration activity
for tungsten and the limited amount of data
and information available, future exploration
activity is likely to benefit greatly from new
regional geophysical and remote sensing
surveys in central East Greenland.
- References Hallenstein, C.P., Pedersen, J. L. 1983. Scheelite Mineralization in Central East Greenland. Mineralium
Deposita 18, p. 315-333.
Harpøth, O., Pedersen, J.L., Schønwandt, H.K. & Thomassen, B. 1986: The mineral occurrences of central
East Greenland, Geoscience 17, 139 pp.
Sørensen, L.L., Stensgaard, B.M. & Rosa, D. 2014: Tungsten potential in Greenland. Geology and Ore, vol.
25, 12 pp.
Close-up of the tungsten deposit located at South Margerie Dal/ Colinedal on Ymer Ø in central East Greenland. Photo: 21st North
ZINC
- Where in Greenland is zinc found and where is
the potential Greenland has an excellent potential for sedimentary exhalative (SEDEX) and Mississippi-Valley type (MVT) zinc and lead deposits. The former tend to be large deposits, found in clastic sedimentary rocks, particularly shales, with reserves and resources in individual deposits exceeding 100 million tonnes and with typical grades of about 10–15% Zn and 2–5% Pb. The latter are hosted in carbonate rocks and tend to be smaller than SEDEX deposits, though they often occur in clusters in a single
district. MVT deposits tend to have lower grades, typically 2–6% Zn and 1–3% Pb, but are of easy beneficiation. In addition to Zn and Pb, these deposit types can yield Ag, Cd, Ge, In, barite, and fluorite as by-products. In addition to these sedimentary zinc deposits, zinc is also found in the unusual context of an alkaline intrusion, in the Kvanefjeld deposit, in South Greenland. At this locality, zinc concentrates are planned to be produced as a by-product of rare earth and uranium mining. Despite its potential, in Greenland zinc has only been mined at the Black Angel MVT mine (West Greenland) and at the Blyklippen mine (East Greenland). In the former, 11.2 million tons at 12.3% Zn were mined between 1973 and 1990, and in the latter and unquantified but small amount of zinc concentrate was produced between 1956 and 1962.
- Known resources and reserves of zinc in Greenland A compilation of the distribution of potential undiscovered and known zinc resources in Greenland is included in the table below. The potential undiscovered Zn resource estimates are derived from a workshop in 2011 on the “Assessment of the zinc potential in Greenland” (Sørensen et al. 2013):
Undiscovered Zn resources (Mt Zn metal) Resources in known deposits
Areas SEDEX MVT Source: Deposits: Ton/grade Type Source:
North Greenland (Franklinian Basin)
13.7 2.7 Sørensen et al (2013) Citronen Fjord
132 Mt @ 4.1% Zn
JORC indicated
Ironbark Zinc
East Greenland (Jameson Land Basin + Krummedal and Eleonore Bay Basin)
1.5 1.4 Sørensen et al (2013)
West Greenland (Karrat Group)
1.2 0.3 Sørensen et al (2013) Black Angel 4.4 Mt @ 8.6% Zn
JORC measured
Angel Mining
Northeast Greenland (Hekla Sund Basin)
2.1 0 Sørensen et al (2013)
Northwest Greenland (Inglefield Land + Thule Basin)
1.6 0.2 Sørensen et al (2013)
South Greenland (Alkaline intrusions)
NA NA Kvanefjeld 956 Mt @ 2.4% Zn
JORC indicated
Greenland Minerals & Energy
- Overview and status of projects exploring for zinc Depressed zinc prices have long subdued exploration for zinc. Furthermore, the capacity of China, the largest world producer, to respond to possible rises in prices with additional output remains a possibility that disincentives exploration. However, the planned closure of several large mines (Brunswick and Perseverance, in Canada; Skorpion, in Namibia, Lisheen, in Ireland; Century, in Australia) has encouraged some major companies (Glencore Xstrata, Nyrstar and Boliden) to recently launch or support zinc exploration projects, until recently of interest mostly to junior companies only. The effects of this change of attitude towards zinc exploration also translated into Greenland. As a result, Boliden signed an agreement with Avannaa to explore for zinc in the Franklinian Basin of North Greenland, namely in Washington Land (Petermann prospect). Glencore Xstrata, on the other hand, is funding Ironbark, who is committed to Greenland, recently finishing a feasibility project for the Citronen Fjord SEDEX deposit and engaged in exploration in Washington Land (Cass Fjord prospect) and Eastern Greenland (Blyklippen area).
Greenland potential
Further developments in exploration initiatives in the most prospective area, the Franklinian Basin of North Greenland, remain however constrained by a temporary closure for new mineral applications in the area north of latitude 81°N due to new nature preservation areas. While current licenses and license applications, namely those held by Ironbark and Avannaa, are not affected and will continue under current license terms, this closure effectively has kept most of Franklinian Basin out of reach for exploration. It is expected, however, that a new set of licensing terms, including definition of the license blocks, will be established soon, possibly prompting a new wave of exploration. In terms of planned production, the most advanced project is the Kvanefjeld project, by Greenland Minerals and Energy, which is directed towards the production of U and rare earth elements but which is planned to have significant zinc produced as a by-product. The feasibility study on the Citronen Fjord deposit, by Ironbark, projects an expected mine life of 14 years, with a production rate of 3.3 Mt/a, with an average zinc grade of 5.85% from the initial underground mining and an average zinc grade of 3.10% from the final open pit mining.
- Recommendations The potential of the Franklinian Basin of North Greenland for zinc, but also germanium and fluorite, warrants dedicated high-resolution geophysical and remote sensing surveys. Recommended surveys include aeromagnetic, gravimetric and hyperspectral surveys covering the whole basin. These surveys can assist in identifying main structures controlling the distribution of mineralisation, which should subsequently be followed-up with field reconnaissance expeditions. These would facilitate and stimulate mineral exploration and possibly lead to new discoveries. A more complete evaluation of the potential of the Franklinian Basin would greatly benefit from funding dedicated to deepening the cooperation with Canada, as this basin extends into this country and several Canadian researchers are engaged in its study. Field work studies, both for research and exploration, require the availability of key logistical platforms in remote areas, particularly in North Greenland. Therefore, the maintenance and possible expansion of facilities such as Station Nord
(operated by the Joint Arctic Command of the Danish Defense) is recommended. Likewise, the availability of an ice-reinforced expedition vessel is also recommended as a means of extending mineral reconnaissance efforts to more remote areas. Finally, to better assess the feasibility of possible future mining projects, a prerequisite to attract mineral exploration, the existence of bathymetry data on the fjords, needed to evaluate locations for deep water ports, would be beneficial. Likewise, research on effective and mobile mining infrastructure / energy supplies in high Arctic areas are strongly recommended.
- References Angel Mining, website: www.angelmining.com Geology and Ore, No 5 – The Blyklippen Mine lead-zinc mine at Mesters Vig, Eastern Greenland, Geological Survey
of Denmark and Greenland, 12 pp. Greenland Minerals and Energy, website: www.ggg.gl Ironbark zinc, website: www.ironbarkgold.com.au/ Sørensen, L.L., Stensgaard, B.M., Thrane, K., Rosa, D. & Kalvig, P. 2013: Sediment-hosted zinc in Greenland -
Reporting the mineral resource assessment workshop 29 November - 1 December 2011, Danmarks og Grønlands Geologiske Undersøgelse Rapport 2013/56, 184 pp.
1
Annex 2: EU industry needs & Greenland raw material deposits
2
CHROMIUM
- Mining sites in Europe Tornio, Kemi (FI)
- European mining companies with national or global activities Cronimet Group (DE)
ENRC (UK)
Outokumpu (FI)
Glencore Xstrata (CH)
- Primary production companies in EU (refiners / smelters) Cronimet Group (DE)
ENRC (UK)
Outokumpu (FI, Chromite)
- Major processing companies in EU (production of semi-products) Plansee (AT)
Delachaux (FR)
Elektrowerk Weisweiler (DE)
Manifold stainless steel mills and stainless steel processing companies
- Relevant association ICDA (International chromium development association)
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
3
- Main products - Applications and end-use
90% of chromium is used in stainless
steel which is an essential material
for large industrial sectors
(automotive, construction,
engineering) Refractory materials Chemical specialty products (e.g.
colours, leather tanning)
- Relevant sectors
Mechanical engineering Automotive Transport Building construction Metallurgical industry Refractories/Foundries chemistry
Figure: End-use of chromium in the USA 2012
Source: Report on critical Raw Materials for the EU, 2014,
Figure 32 on page 31
Figure: World ferrochromium supply and demand forecasts to 2020
(´000s tonnes)
Source: Report on critical Raw Materials for the EU, 2014, Figure 33 on page 32
4
- Future technologies The emerging technologies are not expected to have significant influence on Cr-demand up to 2030:
o Redox flow battery
o Desalination of sea water
o Orthopedic implants
- References
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014
(http://ec.europa.eu/enterprise/policies/raw-materials/critical/index_en.htm
USGS, 2014, Chromium (http://minerals.usgs.gov/minerals/pubs/commodity/chromium/mcs-2014-
chrom.pdf)
Outokumpu-Homepage (www.outokumpu.com)
ARS Mining Homepage (http://www.arsiminen.de/)
Cronimet Homepage (http://www.cronimet.de/en/)
ENRC Homepage (http://www.enrc.com/about-us/glance)
Glencore Xstrata Homepage (http://www.glencorexstrata.com/)
Plansee Homepage (http://www.plansee-group.com/)
Delachaux Homepage (http://www.delachaux.fr/En/)
Elektrowerk Weisweiler GmbH Homepage (http://www.elektrowerk.de/en/index2.html)
ICDA (International chromium development association) Homepage
(http://www.icdacr.com/index.php?lang=en)
ICDA Uses of chrome
(http://www.icdacr.com/index.php?option=com_content&view=article&id=104&Itemid=167&lang=en)
Asian Metal (http://www.asianmetal.com)
USGS, 2011 Minerals Yearbook Chromium; April 2013
(http://minerals.usgs.gov/minerals/pubs/commodity/chromium/myb1-2011-chrom.pdf)
5
COPPER
EU industry* and
applications
- Mining sites in Europe Rudna (PL)
Aguas Tenidas Mine (ES)
Neves-Corvo (PT)
Zinkgruvan (SE)
Aitik (SE)
Garpenberg (SE)
The Boliden Area (SE)
Aguablance (ES)
- European mining companies with national or global activities KGHM Polska Miedź (PL) Boliden (SE)
Lundin Mining Corporation (CA/SE)
Trafigura (UK)
Anglo American (UK)
Rio Tinto (UK)
Cronimet Group (DE)
- Primary production companies in EU (refiners and smelters) Atlantic copper (ES)
Aurubis (DE)
Boliden (SE)
Metallo Chimique (DE)
Montanwerke Brixlegg (AT)
KGHM (PL)
6
- Major processing companies in EU (production of semi-products)
Cupori (FL)
Halcor Metal Works (GR/BG)
KME (DE)
La Fraga (ES)
Luvata (UK)
Mueller Industries (UK)
Nexans (FR)
Wieland (DE)
Cronimet Group (DE)
Mansfelder Kupfer und Messing GmbH (DE)
Numerous small, medium and large enterprises in the end-use manufacturing
- Relevant association European Copper Institute
- Main products - Applications and end-use
Cable
Wires
Transformers
Motors
Electronic components
Switchgear
Tubes
Pipes
Construction
Transport equipment
Plumbing
Air-conditioning
Refrigeration
Figure: End-use of copper in Europe 2011
Source: Study on non Critical Raw Materials at EU Level,
2014, Figure 13 on page 22
- Relevant sectors
Electrical applications Building Construction Automotive and other transport
- Trend Rising demand in all sectors.
7
Exports are an important demand driver since Europe is a net exporter of semi-finished goods.
Europe is a net exporter of semi-finished goods.
- Future technologies Additional demand will arise from electric cars.
- References
Study on non Critical Raw Materials at EU Level, 2014 (http://ec.europa.eu/enterprise/policies/raw-
materials/files/docs/crm-non-critical-material-profiles_en.pdf)
USGS, 2014, Copper (http://minerals.usgs.gov/minerals/pubs/commodity//copper/mcs-2014-coppe.pdf)
ICSG: International Copper Study Group (http://www.icsg.org/)
ICSG The World Copper Factbook 2013 (http://copperalliance.org/wordpress/wp-
content/uploads/2012/01/2013-World-Copper-Factbook.pdf)
Trafigura Homepage (www.trafigura.com)
Lundin Mining Homepage (http://www.lundinmining.com)
Boliden Homepage (http://www.boliden.com/Operations/Mines/)
KGHM Homepage (http://www.kghm.pl/ und andere Homepages)
Anglo American Homepage (http://www.angloamerican.com/)
Rio Tinto Homepage (http://www.riotinto.com/)
Cronimet Group Homepage (http://www.cronimet-mining.com/en/mining/operations/)
Aurubis Homepage (http://www.aurubis.com/)
Metallo Chimique Homepage (http://www.metallo.com)
Montanwerke Brixlegg Homepage (http://www.montanwerke-
brixlegg.com/)
Atlantic Copper Homepage (http://www.atlantic-copper.es)
Wieland Homepage (http://www.wieland.de/)
European Copper Institute (http://www.copperalliance.eu/)
Copper development association (http://www.copperinfo.co.uk/environment/recycling.shtml)
London Metal Exchange (http://www.lme.com/en-gb/metals/non-ferrous/copper/#tab2)
Copper development association: Annual Data 2013. Copper supply & consumption - 1992-2012
8
BGR Deutschland - Rohstoffsituation 2012, November 2013
(http://www.bgr.bund.de/DE/Themen/Min_rohstoffe/Downloads/Rohsit-
2012.pdf?__blob=publicationFile&v=9)
9
GRAPHITE
- Mining sites in Europe Kringel mine (SE)
Skaland mine (NO)
Romania
Kaisersberg (AT)
Data on European production in 2012: Romania: 7.000 t; Norway 7.000 t
Very low in comparison to world production of 1.100.000 t in 2010
- European mining companies with national or global activities IMERYS - timcal (FR)
Norwegian Graphite AS (NO)
Skaland Graphite AS (NO)
Grafitbergbau Kaisersberg (AT)
- Processing companies in the European Union AMG (NL) and subsidiary Kropfmühl (DE)
SGL Carbon SE (DE)
TOKAI ERFTCARBON GmbH (DE)
Numerous end-use manufacturers in Europe, e.g. for batteries: Axeon, Varta, Saft
- Relevant association European Carbon and Graphite Association
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
10
- Main products - Applications and end-use
Electrodes in steel productions
Electrodes in batteries and fuel cells
Furnace lining
Molds for casting
Carbon brushes
Lubricants
Brake linings
Figure: Worldwide use of natural graphite in
2010
Source: Report on critical Raw Materials for the EU, (2014),
Figure 104 on page 104
- Relevant sectors
Steel industry
Construction (building) industry
Automotive industry
Electrical industry
- Applications by type of natural graphite
Natural: Amorphous
(Most abundant type; least valuable;
account for 44% of global
production)
Natural: Flake
(Less common and of higher purity
than amorphous graphite; account for
55% of global production)
Natural: Vein
(most valuable and rarest form of
graphite; accounts for 1% of world
production)
Carbon brushes Heat sinks Coated conductors Refractory applications Brake pads Clutches Foundry applications Steel alloys Lubricant additives Pencils Paints Rubber and polymer
composites Thread compounds
Batteries Carbon brushes Heat sinks Coated conductors Lubricant additives Pencils Refractory applications Graphite shapes Coated conductors brake
pads Clutches Foundry applications Powder metallurgy Drilling mud additives Nuclear reactors Flame retardants
Foundry applications Lubricants Powder metallurgy Electrical components Carbon brushes
11
Synthetic diamonds
- Trend Rising demand in most sectors. Graphite demand is expected to grow in the near future at around
3.4% per year to 2010 (Report on critical Raw Materials for the EU, 2014).
Higher growth is expected for flake grades graphite (for batteries, friction products, lubricants etc).
Rising prices may lead to increasing substitution (e.g. by synthetic graphite).
Li-ion batteries for electric vehicles will be an important demand driver in the mid and long term. A
growth by 25% a year up to 2020 is expected.
Improving refining qualities are likely lead to new high-tech applications
Figure: World natural graphite supply and end-use forecast to 2020
(´000 tonnes)
Source: Report on critical Raw Materials for the EU, 2014, Figure 105 on page 106
- Future technologies Lithium-ion batteries (mobile phones, laptops, tablet computers, electric vehicles) [relevant
demand driver!]
Fuel cells [potentially relevant demand driver!]
Graphene (as a better conductor of heat and electricity than copper – for electronics, solar cells etc)
Vanadium redox batteries
Pebble bed nuclear reactors
In R&D: carbon nanotubes in electronics, solar cells, hydrogen storage and others
12
- References
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014
(http://ec.europa.eu/enterprise/policies/raw-materials/critical/index_en.htm)
USGS 2014, Graphite (http://minerals.usgs.gov/minerals/pubs/commodity/graphite/mcs‐2014‐graph.pdf)
Report on Substitution of Critical Raw Materials, CRM_InnoNet; D3.3 Raw material profile, September
2013
Flinders Resources Homepage (http://www.flindersresources.com/s/NewsReleases.asp?ReportID=509924)
Industrial Minerals Report: The Natural Graphite Industry in 2012 (http://americanresources.org/wp-
content/uploads/2012/12/Industrial-Minerals-Data-Report.pdf)
Homepage IMERYS (http://www.imerys.com/scopi/group/imeryscom/imeryscom.nsf/pagesref/SBDD-
8QGETA?OpenDocument&Lang=EN)
Homepage AMG (http://www.amg-nv.com/Home/default.aspx)
Homepage SGL Group (http://www.sglgroup.com/cms/international/company/index.html?__locale=en)
Homepage TOKAI ERFTCARBON GmbH (http://www.tokai-erftcarbon.com/en/)
Homepage European Carbon and Graphite Association (http://www.carbonandgraphite.org/)
13
IRON
- Mining sites in Europe Malmberget (SE)
Very small iron ore mining in Austria, the Slova Republic and Germany
- European mining companies with national or global activities LKAB Minerals (SE)
Anglo American (UK)
Rio Tinto (UK)
London mining (UK)
- Primary production companies in EU (refiners and smelters) There are more than 50 steel works in EU-28 and numerous iron foundries.
- Major processing companies in EU (production of semi-products): There are numerous large companies in the processing of steel and iron materials in sectors such as
o Automotive
o Construction
o Mechanical engineering
o Infrastructure
o etc.
- Relevant association EUROFER (European Steel Assocation)
EUROmetal
CAEF (European Foundry Association)
EUROALLIAGES
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
14
- Main products - Applications and end-use
"Nothing is manufactured, processed or
transported without steel" - due to the large
number of products no main products are
listed here
Figure: End-use of iron in Europe in 2010
Source: Study on non Critical Raw Materials at EU Level,
2014, Figure 28 on page 44
- Relevant sectors
Automotive & transport Construction Engineering Tubes Infrastructure Domestic applicances
- Trend Rising demand in proportion to the GDP.
The demand for stainless steel, is expected to increase in the range of 4-5% per year to 2020.
- References
USGS 2014, Iron Ore (http://minerals.usgs.gov/minerals/pubs/commodity/iron_ore/)
Macro business: A brief history of iron ore markets, from August 2013, retrieved April 2014
(http://www.macrobusiness.com.au/2013/08/a-brief-history-of-iron-ore-markets/)
BGR Deutschland - Rohstoffsituation 2012, November 2013
(http://www.bgr.bund.de/DE/Themen/Min_rohstoffe/Downloads/Rohsit-
2012.pdf?__blob=publicationFile&v=9)
Homepage EUROFER (European Steel Association) (http://www.eurofer.org/)
Homepage EUROmetal (The voice of European steel, tubes and metal intermediation)
(http://www.eurometal.net/)
Homepage CAEF (European Foundry Association) (http://www.caef.org/default.asp)
Homepage EUROALLIAGES (European Association of ferro-alloys and silicon producers)
15
(http://www.euroalliages.com/)
World steel consumption 2012 (http://www.steelonthenet.com/consumption.html)
World Steel Association, Steel Applications, retrieved on 13May2014
(http://www.steeluniversity.org/content/html/eng/default.asp?catid=2&pageid=-424514437)
World Steel Association, Fact sheet The three Rs, retrieved on 13May 2014
(http://www.worldsteel.org/dms/internetDocumentList/fact-sheets/Fact-
sheet_3Rs/document/Fact%20sheet_3Rs.pdf)
World Steel Association, World steel in figures 2013
(http://www.worldsteel.org/dms/internetDocumentList/bookshop/Word-Steel-in-Figures-
2013/document/World%20Steel%20in%20Figures%202013.pdf)
World Steel Association, Fact Sheet Raw Materials
(http://www.worldsteel.org/dms/internetDocumentList/fact-sheets/Fact-sheet_Raw-
materials2011/document/Fact%20sheet_Raw%20materials2011.pdf)
Study on non Critical Raw Materials at EU Level, 2014 (http://ec.europa.eu/enterprise/policies/raw-
materials/files/docs/crm-non-critical-material-profiles_en.pdf)
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014
(http://ec.europa.eu/enterprise/policies/raw-materials/critical/index_en.htm
16
NIOBIUM
- Mining sites in Europe No mining sites in EU (only scrap available as raw material source)
- European mining companies with global activities Anglo American (UK)
Eramet (FR)
- Primary production companies in EU (refiners and smelters) No primary niobium production in Europe, but production of niobium alloys from recycling (e.g.
Cronimet (DE))
- Major processing companies in EU (production of semi-products) H.C. Starck (DE)
A&M Group Ltd (UK)
AMC Group (UK)
Heraeus (DE)
All steel works
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
17
Figure: Supply chain map of niobium
Source: Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014, Figure 106 on
page 109
- Relevant associations
Tantalum-Niobium International Study Center (TIC)
- Main products - Applications and end-use
Ferro-niobium largest market for
niobium (90% of worldwide niobium
demand) High-strength and corrosion resistant
steel
Specific alloys, chemicals
- Relevant sectors
Construction (high-strength low alloy
steel) Automotive (HSLA steel) Oil and gas supply (HSLA steel) Nuclear industry (alloys) Aircraft industry (alloys) Chemistry
Figure: Worldwide end-use of niobium
Source: Report on critical Raw Materials for the EU, (2014),
Figure 111 on page 114
18
- Trend Growing demand (analogous to the rising steel demand)
The world outlook for ferro-niobium demand is expected to increase by around 8% per year due to
rising global demand for steel in construction, infrastructure and automotive applications as well as
trend towards greater use of HSLA steel.
Figure: World ferro-niobium capacity and consumption forecast to 2020 (´000
tonnes)
Source: Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014, Figure 112
on page 115
- Future technologies The future Nb-demand will highly depend on the future steel demand.
Future technologies are assumed to require much lower amounts of Nb:
o miniaturized capacitators
o supraconductors in medical and research applications
19
- References
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014 (http://ec.europa.eu/enterprise
materials/critical/index_en.htm
http://www.oakdenehollins.co.uk/media/308/Critical_Metals_Decarbonisation.pdf, page 101
Critical raw materials for the EU, 2010, http://ec.europa.eu/enterprise/policies/raw-materials/files/docs/report-b_en.pd
Mineral Commodity Summaries: Niobium, U.S. Geological Survey, 2014
Anglo American Homepage: http://www.angloamerican.com/
H.C. Starck Homepage: http://www.hcstarck.com/de/home.html
A&M Group Ltd Homepage: http://www.amgroup.uk.com/
TIC: wordwide association representing the tantalum and niobium industry http://tanb.org/
Report on Substitution of Critical Raw Materials, CRM_InnoNet; D3.3 Raw material profile, September 2013
AMC Group Homepage: http://www.amcgroup.com/
Asian Metals Homepage: http://www.asianmetal.com/
Eramet Homepage: http://www.eramet.com/
USGS 2011 Minerals Yearbook Niobium and Tantalum (http://minerals.usgs.gov/minerals/pubs/commodity/niob
niobi.pdf)
CBMM Homepage Operations (http://www.cbmm.com/us/p/76/operations.aspx)
Fraunhofer Institut 2009: Rohstoffe für Zukunftstechnologien
20
TANTALUM
- Mining sites in Europe No mining sites in Europe
- European mining companies with global activities No European mining companies
- Primary production companies in EU (refiners and smelters) H.C. Starck (DE)
Advances Metallurgical Group (NL)
Plansee (AT)
Treibacher (AT)
Heraeus (DE)
- Major processing companies in EU (production of semi-products) Plansee (AT)
H.C. Starck (DE)
Tantec (DE)
EPCOS (DE/PT)
Tantaline (DK)
Hitachi Europe
- Relvant associations: TIC (Tantalum-Niobium International Study Center)
Minor metals trade association
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
21
- Main products - Applications and end-use
Tantalum capacitators
High-temperature resistant materials
(e.g. for aicraft engines)
Corrosion resistant materials
High-strength steels and carbides
(cutting tools)
Sputtering targets for semiconductor
components
Surface acoustic wave filters
Chemical apparatus engineering
Laboratory equipment
- Relevant sectors
Electronics Automotive Aerospace Medicine Optical industry Chemical industry
Figure: Worldwide end-use of tantalum in 2011
Source: Study on non Critical Raw Materials at EU Level,
2014, Figure 60 on page 102
- Trend Roskill assumes a slow but steady growth in demand with highest growth rates in the segments
superalloys, sputtering targets and tantalum chemicals.
- Future technologies Tantalum is already used in a wide range of high-tech technologies which are expected to develop
further.
Besides these manifold applications, no mass-relevant additional future field was identified.
22
- References
Study on non Critical Raw Materials at EU Level, 2014 (http://ec.europa.eu/enterprise/policies/raw-
materials/files/docs/crm-non-critical-material-profiles_en.pdf)
USGS 2014, tantalum http://minerals.usgs.gov/minerals/pubs/commodity/niobium/
Report on Substitution of Critical Raw Materials, CRM_InnoNet; D3.3 Raw material profile, September
2013
Plansee Homepage: http://www.plansee-group.com/
H.C. Starck Homepage: http://www.hcstarck.com/de/home.html
Tantec Homepage: http://www.tantec-online.de/en_index.php?lang=en
A&M Group Ltd Homepage: http://www.amgroup.uk.com/
AMC Group Homepage: http://www.amcgroup.com/
Tantalum-Niobium International Study Center Homepage: http://tanb.org/
Minor metals Trade Assocation Homepage: http://www.mmta.co.uk/
AnnexV, critical raw materials for the EU 2010, page 193 (http://ec.europa.eu/enterprise/policies/raw-
materials/files/docs/annex-v_en.pdf)
Polinares EU Policy on Natural Resources, Fact Sheet: Tantalum; March 2012
(http://www.polinares.eu/docs/d2-1/polinares_wp2_annex2_factsheet2_v1_10.pdf)
Assessment of due diligence compliance cost, benefit and related effects on selected operators in relation to
the responsible sourcing of selected minerals; European Commission, September 2013
(http://trade.ec.europa.eu/doclib/docs/2014/march/tradoc_152230.pdf)
ERAMET (http://www.eramet.com/sites/default/files/cp/resultats2013_eramet_21_02_2014_fr.pdf)
USGS 2013, An Exploration in Mineral Supply Chain Mapping Using Tantalum as an Example
(http://pubs.usgs.gov/of/2013/1239/pdf/ofr2013-1239.pdf)
Minor metals Trade Assocation (editor); authors: Patrick Stratton, Roskill Information Services and David
Henderson, Rittenhouse International: Tantalum Market Overview; http://www.mmta.co.uk/
23
PGEs
- Mining sites in Europe No mining sites in EU
- European mining companies with national or global activities Anglo American (UK)
Lonmin (UK)
Cronimet (DE)
- Primary production companies in EU (refiners and smelters) Johnson Matthey (UK)
Heraeus (DE
H.C. Starck (DE)
Chimet (IT)
Anglo American (UK)
Glencore Xstrata (CH, UK)
- Major processing companies in EU (production of semi-products): Umicore (BE)
Johnson Matthey (UK)
Heraeus (DE)
BASF (DE)
Heimerle+Meule Group (DE)
- Relevant association EPMF (European Precious Metals Federation)
International Platinum Group Metals Association
ECMA (European Catalyst Manufacturers Association)
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
24
- Main products - Applications and end-use
Autocatalysts
Catalysts in chemical industry
Jewellery
Alloys for electronic components
Medical products
Catalysts in fuel cells
Financial investment
- Relevant sectors
Automotive Chemical industry Electronicsl Medical technology Jewellery Finance
Figure: Word demand for PGMs for 2012
Source: Report on critical Raw Materials for the EU, 2014,
Table 36 on page129
Figure: World natural graphite supply and end-use forecast to 2020
(´000 tonnes)
Source: Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014, Figure 126 on
page 131
25
26
- Trend
Rising demand in all sectors.
Overall strong demand is expected for platinum, palladium and rhodium at around 4-5 % per year.
The strongest increase is expected in the autocatalysts market.
The demand for platinum jewellery is also expected to remain strong, particularly in China.
- Future technologies Lithium-ion batteries (mobile phones, laptops, tablet computers, electric vehicles) [relevant
demand driver!]
Fuel cells [potentially relevant demand driver!]
Graphene (as a better conductor of heat and electricity than copper – for electronics, solar cells, etc.)
Vanadium redox batteries
Pebble bed nuclear reactors
In R&D: carbon nanotubes in electronics, solar cells, hydrogen storage and others
- References
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014
(http://ec.europa.eu/enterprise/policies/raw-materials/critical/index_en.htm
USGS 2014, Platinum-Group Metals; http://minerals.usgs.gov/minerals/pubs/commodity/platinum/
Anglo American Homepage: http://www.angloamerican.com/
Lonmin Homepage: http://www.lonmin.com/
Cronimet Homepage: http://www.cronimet.de/en/
Aurubis Homepage: http://www.aurubis.com/
KGHM Homepage: http://www.kghm.pl/
Umicore Homepage: http://www.umicore.com/en/
Johnson Matthey Homepage: http://www.matthey.com/
Heraeus Homepage: http://heraeus-precious-metals.com/
BASF Homepage: http://www.deutschland.basf.com/ecp3/Germany/en/content/aboutus/index
H.C. Starck Homepage: http://www.hcstarck.com/de/home.html
EPMF Homepage: http://www.epmf.be/
International Platinum Group Metals Association Homepage: www.ipa-news.com
ECMA Homepage: http://www.cefic.org
Johnson Matthey Prices retrieved 22nd April 2014 (http://www.platinum.matthey.com/prices/price-charts)
27
NEODYMIUM
- Mining sites in Europe Project in pre-mining phase: Norra Kärr (SE) by Tasman metals (Canadian company with Swedish
subsidiary) Skaland mine (NO)
- European mining companies with global activities (all projects are still
in the pre-mining phase!): Avannaa Resources (UK)
Rare Earths Minerals (UK)
CGRG Ltd. (CZ)
- Primary production companies in EU (refiners and smelters) No primary production from ores in Europe
The French Rhodia (Solvay Group) processes smaller amounts of high-concentrated rare earths
oxides.
- Major processing companies in EU (production of semi-products) Solvay (BE/FR) (former Rhodia)
Vacuumschmelze (DE)
Silmet/Molycorp (EE, subsidiary of US Molycorp)
Arnold Magnetic Technologies (UK)
Less Common Metals (UK, subsidiary of Canadian GWMG)
Goudsmit Magnetic Systems (NL)
Siemens AG (DE)
ALSTOM (FR)
BASF (DE)
Treibacher (AT)
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
28
- Main products - Applications and end-use
Large wind turbines with direct gears
Motors for hybrid vehicles
Motors for electric vehicles
Permanent magnets in industrial and
household applications (e.g. energy
efficient washing machines)
Hard disk drives
Loud speakers
NiMH-batteries
Figure: Neodymium end-use, 2012
Source: Report on critical Raw Materials for the EU, 2014,
Figure 169 on page 166
- Relevant sectors
Wind energy Automotive Mechanical engineering
Electronics
- Trend Worldwide rising demand in wind power and automotive industry, particularly in Chinese wind
power installations.
The global neodymium demand is expected to increase by around 7% per year according to the 2014
report on critical materials for the EU.
29
Figure: World neodymium supply and demand forecast to 2020 (tonnes)
Source: Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014, Figure 170 on
page 167
- Future technologies Motors for e-mobility
Large wind turbines with direct gear
- References
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014
(http://ec.europa.eu/enterprise/policies/raw-materials/critical/index_en.htm
USGS 2014 (http://minerals.usgs.gov/minerals/pubs/commodity/rare_earths/mcs-2014-raree.pdf)
UNEP International Resource Panel 2011, Recycling Rates of Metals: A status report
Asian Metals, retrieved on 22nd April 2014 (http://www.asianmetal.com)
Schüler et al, Study on Rare Earths and Their Recycling, 2011
ALKANE Resources Ltd.: Chart on rare earth resource by country excluding China, published on the
website http://www.australianrareearths.com/current-issues.html, download at 04 Nov 2010
Ministry of Environmental Protection In: The Explanation of Compiling Emission Standards of Pollutants
30
from Rare Earths Industry 2009 viewed 11 October 2010,
Tansman metals Homepage (http://www.tasmanmetals.com/s/REEProjects.asp)
Avannaa Resources Homepage (http://www.avannaa.com)
Rare Earth Minerals Homepage (http://www.rareearthmineralsplc.com/)
CGRC Homepage (http://www.cgrg.cz/)
Nuna Minerals Homepage (http://www.nunaminerals.com/)
Vacuumschmelze Homepage (http://www.vacuumschmelze.com/index.php?id=30)
Arnold magnetic Technologies Homepage (http://www.arnoldmagnetics.com/)
Solvay Homepage (http://www.solvay.com/)
Treibacher Industrie AG Homepage (http://www.treibacher.at/de/home.html)
Goudsmit Magnetic Systems Homepage (http://www.goudsmit-magnetics.nl/EN/)
Siemens AG Homepage (http://www.siemens.com)
ALSTOM Homepage (http://www.alstom.com/)
Osram Homepage (http://www.osram.de/osram_de/)
Philips Homepage (http://www.philips.co.uk/?locale_org=de_de)
BASF Homepage (http://www.deutschland.basf.com/ecp3/Germany/en/content/aboutus/index)
ERECON (European Rare Earths Competence Network Homepage
http://ec.europa.eu/enterprise/policies/raw-materials/erecon/index_en.htm)
Lynas annual report 2013
(https://www.lynascorp.com/Annual%20Reports/Lynas_Annual%20Report_2013%20FINAL%201272078.
pdf)
CRS Report for Congress: Rare Earth Elements: The Global Supply Chain, December 2013
(http://www.fas.org/sgp/crs/natsec/R41347.pdf)
31
DYSPROSIUM
- Mining sites in Europe Project in pre-mining phase: Norra Kärr (SE) by Tasman metals (Canadian company with Swedish
subsidiary)
- European exploration companies with global activities (all projects
are still in the pre-mining phase!): Avannaa Resources (UK)
Rare Earths Minerals (UK)
CGRG Ltd. (CZ)
- Primary production companies in EU (refiners and smelters): No primary production from ores in Europe
The French Rhodia (Solvay Group) processes smaller amounts of high-concentrated rare earths
oxides.
- Major processing companies in EU (production of semi-products): Solvay (BE/FR) (former Rhodia)
Vacuumschmelze (DE)
Silmet/Molycorp (EE, subsidiary of US Molycorp)
Arnold Magnetic Technologies (UK)
Less Common Metals (UK, subsidiary of Canadian GWMG)
Goudsmit Magnetic Systems (NL)
Siemens AG (DE)
ALSTOM (FR)
Treibacher (AT)
- Relevant association ERECON (European Rare Earths Competency Network)
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
32
- Main products - Applications and end-use
Motors for hybrid vehicles Motors for electric vehicles Large wind turbines with direct
gears Laser (small amounts) Nuclear reactor control (small
amounts)
Figure: Dysprosium end-use, 2012
Source: Report on critical Raw Materials for the EU, 2014,
Figure 184 on page 176
- Relevant sectors
Automotive Wind energy Nuclear and optical industry (small
amounts)
- Trend
Worldwide rising demand in wind power and automotive industry, particularly in Chinese wind
power installations.
The global dysprosium demand is expected to increase by around 9% per year according to the 2014
report on critical materials for the EU.
The recent developments of permanent magnets for high-temperature applications with a lower
dysprosium content (savings of 30-50 %) may slow down this trend.
Figure: World dysprosium supply and demand forecast to 2020 (tonnes)
33
Source: Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014, Figure 185 on
page 177
- Future technology
Motors for e-mobility
Large wind turbines with direct gear
- References
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014
(http://ec.europa.eu/enterprise/policies/raw-materials/critical/index_en.htm
USGS 2014 (http://minerals.usgs.gov/minerals/pubs/commodity/rare_earths/mcs-2014-raree.pdf)
UNEP International Resource Panel 2011, Recycling Rates of Metals: A status report
Asian Metals, retrieved on 22nd April 2014 (http://www.asianmetal.com)
Schüler et al, Study on Rare Earths and Their Recycling, 2011
ALKANE Resources Ltd.: Chart on rare earth resource by country excluding China, published on the
website http://www.australianrareearths.com/current-issues.html, download at 04 Nov 2010
Ministry of Environmental Protection In: The Explanation of Compiling Emission Standards of Pollutants
from Rare Earths Industry 2009 viewed 11 October 2010,
Tansman metals Homepage (http://www.tasmanmetals.com/s/REEProjects.asp)
Avannaa Resources Homepage (http://www.avannaa.com)
Rare Earth Minerals Homepage (http://www.rareearthmineralsplc.com/)
CGRC Homepage (http://www.cgrg.cz/)
Nuna Minerals Homepage (http://www.nunaminerals.com/)
Vacuumschmelze Homepage (http://www.vacuumschmelze.com/index.php?id=30)
Arnold magnetic Technologies Homepage (http://www.arnoldmagnetics.com/)
Solvay Homepage (http://www.solvay.com/)
Treibacher Industrie AG Homepage (http://www.treibacher.at/de/home.html)
Goudsmit Magnetic Systems Homepage (http://www.goudsmit-magnetics.nl/EN/)
Siemens AG Homepage (http://www.siemens.com)
ALSTOM Homepage (http://www.alstom.com/)
Osram Homepage (http://www.osram.de/osram_de/)
34
Philips Homepage (http://www.philips.co.uk/?locale_org=de_de)
BASF Homepage (http://www.deutschland.basf.com/ecp3/Germany/en/content/aboutus/index)
ERECON (European Rare Earths Competence Network Homepage
http://ec.europa.eu/enterprise/policies/raw-materials/erecon/index_en.htm)
Avalon Enters into Rare Earth Refining Agreement and Strategic Partnership, March 2014,
(http://web.tmxmoney.com/article.php?newsid=66144515&qm_symbol=AVL)
35
TUNGSTEN
- Mining sites in Europe Barruecopardo Tungsten project (ES)
Panasqueira mine (PT)
Mining in Mittersill (AT, Salburg)
Property Pöhla-Globenstein (DE)
Canadian companies operate mines in Portugal
- European mining companies with national or global activities Ormonde Mining Plc (IE)
Sojitz Beralt Tin & Wolfram (PT)
Wolfram Bergbau- und Hutten AG (AT)
SME Saxony Minerals and Exploration AG (DE)
Tasman (CA/SE)
- Primary production companies in EU (refiners and smelters) Wolfram Bergbau- und Hutten AG (AT)
Cronimet (DE)
SME Saxony Minerals and Exploration AG (DE)
- Major processing companies in EU (production of semi-products) Plansee (AT)
A&M Group Ltd. (UK)
AMC Group (UK)
Eurotungstene metal powders (FR)
Umicore (BE; silver-tungsten carbide)
- Relevant association ITIA (International Tungsten Industry Association)
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
36
- Main products - Applications and end-use
Corrosion-resistant materials
Lighting technology
High-temperature resistant materials
(e.g. furnaces, power stations)
Extremely hard cutting tools
Materials with high density
Vibration motor of mobile phone
Space travel and aircraft devices
Laser technology
- Relevant sectors
Construction and mechanical
engineering Mining Military Electronics
Figure: Worldwide end-use of tungsten in 2010
Source: Report on critical Raw Materials for the EU, 2014,
Figure 211 on page 199
- Trend Overall market growth is expected to be strong with an annual growth forecast at around 4.5% per
year to 2020.
The tungsten chemicals sector is expected to double by 2020.
The more established cemented carbides, steel alloy and tungsten products will increase more
moderate at 3% - 4% per year.
Overall, the production is expected to increase due to development projects mainly in Europe, North
America and Australia.
By 2017 and 2020 demand is expected to catch up the increased supply.
37
Figure: World total tungsten supply and end-use forecasts to 2020 (tonnes)
Source: Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014, Figure 212 on
page 200
- Future technologies No additional future technologies identified.
However, the listed application fields (high-temperature resistant and corrosion-resistant materials
and extremely hard cutting tools) will expand to more sophisticated application fields (e.g. deep
drilling for raw materials).
38
- References
Report on critical Raw Materials for the EU - Critical Raw Materials Profiles, 2014
(http://ec.europa.eu/enterprise/policies/raw-materials/critical/index_en.htm
European Commission: Critical metals in the path towards the decarbonisatio of the EU Energy sector
http://www.oakdenehollins.co.uk/media/308/Critical_Metals_Decarbonisation.pdf, page 101
Critical raw materials for the EU, 2010, http://ec.europa.eu/enterprise/policies/raw-
materials/files/docs/report-b_en.pdf
Mineral Commodity Summaries: Tungsten, U.S. Geological Survey, 2014
Ormonde Mining Plc.: http://www.ormondemining.com/
Sojitz Beralt Tin & Wolfram: no company homepage http://www.itia.info/sojitz-beralt-tin-wolfram-
portugal-sa.html
Wolfram Bergbau- und Hutten AG: http://www.wolfram.at/wolfram_at/wEnglisch/index.html
SME Saxony Minerals and Exploration AG: http://www.smeag.de/
Report on Substitution of Critical Raw Materials, CRM_InnoNet; D3.3 Raw material profile, September
2013
ITIA (International Tungsten Industry Association); www.itia.info
Plansee Homepage: http://www.plansee-group.com/
A&M Group Ltd Homepage: http://www.amgroup.uk.com/
AMC Group Homepage: http://www.amcgroup.com/
Eurotungstene metal powders Homepage: http://www.eurotungstene.com/
Umicore Homepage: http://www.umicore.com/en/
Asian Metal retrieved 22nd April 2014 (http://www.asianmetal.com)
Tasman Metals (http://www.tasmanmetals.com/s/Projects.asp)
Metal Pages: Word Tungsten Report, September 2012
39
ZINC
- Mining sites in Europe Navan Tara Mine (IE)
Garpenberg (SE)
Boliden Area (SE)
Neves-Corvo (PT
Zinkgruvan (SE)
Aguas Tenidas Mine (ES)
Pyhäsalmi (FI)
Lisheen (IE)
Galmoy (IE)
- European mining companies with national or global activities Boliden (SE)
Lundin Mining Corp. (CA/SE)
Trafigura (UK)
Nyrstar (CH)
Glencore Xstrata (CH)
- Primary production companies in EU (refiners / smelters) Boliden (SE)
Glencore Xstrata (CH)
Nyrstar (CH)
HCM S.A. (PL)
KCM 2000 Group (BG)
ZGH Bolesław (PL) Sometra (RO)
- Major processing companies in EU (production of semi-products) Grillo Werke (DE)
Rheinzink (DE)
Umicore (BE)
Numerous galvanizing plants and foundries
EU industry* and
applications
* Including EU-28, and Norway and Switzerland
40
- Relevant association IZA-Europe (International Zinc Association Europe
- Main products - Applications and end-use
Galvanized steel products (e.g. car
body, ventilation ducts, facade
elements) Brass products (e.g. door handle,
fittings etc.) Die castings for automobiles Rolled zinc (e.g. US Penny) Chemicals (e.g. paints,
pharmaceutical, animal feed)
- Relevant sectors
Building construction Mechanical engineering Automotive and transport Consumer goods Electrical appliances
Figure: Worldwide use of zinc
Source: Study on non Critical Raw Materials at EU Level,
2014, Figure 71 on page 122
- Trend
Rising demand.
Major global drivers will be the increasing demand of zinc for galvanizing steel from construction
sector, demand of zinc alloys and die-casting in automobile sector, and investment in infrastructure
development.
- Future technologies Zinc-air-batteries
41
- References
Study on non Critical Raw Materials at EU Level, 2014 (http://ec.europa.eu/enterprise/policies/raw-
materials/files/docs/crm-non-critical-material-profiles_en.pdf)
Business line (http://www.thehindubusinessline.com/features/investment-world/market-strategy/excess-
supply-to-keep-zinc-price-ranged/article5358571.ece)
USGS 2014, Zinc (http://minerals.usgs.gov/minerals/pubs/commodity/zinc/mcs-2014-zinc.pdf)
Boliden Homepage (www.boliden.com)
Lundin mining Homepage (http://www.lundinmining.com/s/Home.asp)
Trafigura Homepage (www.trafigura.com)
First quantum Homepage (www.first-quantum.com)
IZA-Europe (International Zinc Association Europe) Homepage (http://www.zinc.org/about/profile)
Minerals Education Coalition Homepage (http://www.mineralseducationcoalition.org/minerals/zinc), retrieved
on 16th April 2014
Asian Metal, retrieved 22nd April 2014 (http://www.asianmetal.com)
HCM S.A. Homepage (http://www.hcm.com.pl)
Sometra Homepage (http://www.sometra.ro)
Recyclex Homepage (http://www.recylex.com/)
Umicore Homepage (http://www.umicore.com/en/)
KCM 2000 Group Homepage (http://www.kcm2000.bg)
Ecorys 2011: Competitiveness of the EU Non-ferrous Metals Industries
(http://ec.europa.eu/enterprise/sectors/metals-minerals/files/fn97624_nfm_final_report_5_april_en.pdf)
Minerals Ireland Exploration & Mining Divison Homepage: Current Mining in Ireland, retrieved 26th August
2014 (http://www.mineralsireland.ie/Mining+in+Ireland/Current+Mining.htm)
Market Research Homepage: Global Zinc Industry 2013-2018: Trend, Profit, and Forecast Analysis; retrieved
26th August 2014 (http://www.marketresearch.com/Lucintel-v2747/Global-Zinc-Trend-Profit-Forecast-
7504078/)