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Geology and Cu-Ni-PGE Geology and Cu-Ni-PGE Deposits of the Duluth Deposits of the Duluth Complex, NE MinnesotaComplex, NE Minnesota
Jim MillerDepartment of Geological Sciences
Precambrian Research Center (NRRI)University of Minnesota Duluth
A Looming A Looming StewardshiStewardship Question p Question
for for MinnesotaMinnesota
ns:ns:
When should we
develop this immense copper-nickel-
precious metal
mineral resource?
Talk Outline
Geological origin of the Duluth Complex
Cause and character of the Cu-Ni-PGE sulfide mineralization
World-class ore deposit by any measure
_______________
THE THE MIDCONTINENMIDCONTINENT RIFTT RIFT_______________An attempt at continental rifting 1.1 billion years ago
A. Rift Magmatism
Gabbro
MantlePlume
BasaltFlows
CrustMantle
B. Sediment Infilling Sandstone
C. Compression
1,109-1,086 Ma
1,090-900 Ma
1,000-900 Ma
Tectonic and Tectonic and Magmatic Evolution of Magmatic Evolution of the Midcontinent Riftthe Midcontinent Rift
Midcontinent Rift Midcontinent Rift Geology in the Geology in the Lake Superior Lake Superior
RegionRegion
DuluthComplex
Partridge Partridge River River IntrusionIntrusion
South South KawishiwKawishiwi i IntrusionIntrusion
Sulfur Contamination creating the Cu-Sulfur Contamination creating the Cu-Ni-PGE Sulfide Deposits of the Duluth Ni-PGE Sulfide Deposits of the Duluth
ComplexComplexSSCu Ni Co Pd + Pt + Au
SS
Copper-Nickel-Precious Copper-Nickel-Precious Metal Deposits of the Metal Deposits of the Duluth ComplexDuluth Complex
Average GradesCu – 0.6%Ni - 0.2%Co – 0.005%Pd+Pt+Au – 500-1000 ppb
Based on Severson (1994)
Igneous Stratigraphy of the PRI and Igneous Stratigraphy of the PRI and SKISKI
$/t
on
Cu Prices 1948-2006
Cu-Ni Regional Study
1985 PGE discovered
1999 LTV shuts down
1948 Cu-Ni sulfide discovered at Spruce Rd
1954 INCO drills Maturi
1958 Bear Creek drills
Babbitt
1966 State lands open for mineral
leasingActive exploration
drilling Polymet, Teck, Franconia, Wallbridge
(Duluth Metals)
State land closed to new mineral leasing
Current $ - 7,060
History of ExplorationHistory of ExplorationFrom Severson,2008
Current Exploration ActivityPolymet – NorthmetTeck American – MesabaDuluth Metals – Nokomis, Maturi, Dunka Pit, Birch Lake, Spruce Rd Encampment– South Filson Cr.
The Current SituationThe Current Situation
Chalcopyrite - CuFeS2
Bornite - Cu5FeS4
Cobaltite - CoAsS
Chalcocite - Cu2S
Pentlandite - (Fe,Ni)9S8
Dominant Mineralogyof Magmatic Cu-Ni Sulfide DepositsPyrrohotite – FeS1-x
Talnakhite – Cu9(Fe,Ni)8S16
Why Sulfide Mining?Most of the world’s metals comes from sulfide minerals
ChalcopyriteCuFeS2
BorniteCu5FeS4
CobaltiteCoAsS
SphaleriteZnS
GalenaPbS
ChalcociteCu2S
MolybdeniteMoS2
Pentlandite(Fe,Ni)9S8
CinnabarHgS
The Environmental ChallengePreventing Acid Rock Drainage (ARD)
2FeS2(s) + 7O2(g) + 2H2O(l) →
2Fe2+(aq) + 4SO42-(aq) + 4H+(aq)
Precious Metal MineralsPrecious Metal MineralsPMM Name Formula Total #
Total PMM In Sulfide
Sulfide Host Mineral
cp pn cb po tn bn
Kotulskite Pd(Bi,Te)1-2 15 8 8 0 0 0 0 0
Froodite PdBi2 11 10 3 6 1 0 0 0
Naldrettite Pd2Sb 3 3 3 0 0 0 0 0
Paolovite Pd2Sn 83 68 45 10 7 4 1 1
Sobolevskite PdBi 2 2 1 0 0 0 1 0
Sperrylite PtAs2 26 22 13 5 3 1 0 0
Stibiopalladinite Pd5Sb2 11 5 4 1 0 0 0 0
Taimyrite (Pd,Pt,Cu)3Sn 2 2 2 0 0 0 0 0
Telluropalladinite Pd9Te4 1 1 1 0 0 0 0 0
Undetermined PGM 93 68 31 24 3 4 3 3
Silver sulfide AgS 16 11 7 3 1 0 0 0
Empressite AgTe 2 2 1 0 0 1 0 0
Hessite Ag2Te 3 3 1 1 1 0 0 0
Electrum AuAg 62 22 12 3 3 3 1 0
Gold Au 17 7 3 1 0 3 0 0
TOTALS 347 234 135 54 19 16 6 4
% 67% 57% 23% 8% 7% 3% 2%
PMM study of NorthMet ore, Cervin, 2011
PMM-Sulfide Connection PMM-Sulfide Connection /Disconnection/Disconnection
PdSn
cp
bn sperrylite
cp
pn
pn
cb
cp
cppn
cpx
bt
chl
cp
PdBi PdSbBi
cp
pn plagioclase
cp
Cervin, 2011
Deuteric alteration seperates PMM from host sulfide – implications for beneficiation
Styles of Mineralizatio
nafter Peterson (2001)
• Open (early)– vertically extensive (>
450 meters)– low - mod Cu-Ni grades
and very low Au+PGE– Cu-Ni grades typically
increase towards the basal contact
• Confined (late)– vertically restricted (<
150 meters) – mod - high Cu-Ni grades
and mod to high Au+PGE
– Cu-Ni grades typically are the highest near the top of the mineralized zone
100% Sulfide Plots of SKI Open vs. 100% Sulfide Plots of SKI Open vs. Confined Styles of MineralizationConfined Styles of Mineralization
Deposits
Spruce RdDunka PitSerpentine
Deposits
NokomisMaturiBirch Lake
Open StyleN = 1,737
Open StyleN = 1,737
Confined StyleN = 13,868
Confined StyleN = 13,868
Peterson, 2012
Emplacement/Mineralization Emplacement/Mineralization Model for the South Kawishiwi Model for the South Kawishiwi
IntrusionIntrusion
Peterson, 2012
World Class Ores of the Duluth ComplexWorld Class Ores of the Duluth Complex
#1 or 2 in contained Copper#4 in contained PGE#3 in contained Nickel
Compared to other Magmatic Sulfide Deposits, the Duluth Complex is:
Only the Bushveld, Great
Dyke, and Noril’sk contain more PGE
From Peterson, 2010
World Class Scale of the World Class Scale of the Maturi Deposit AloneMaturi Deposit Alone
Nokomis
From Peterson, 2010 and DM press release
12/2012
Maturi
Maturi
Maturi
The Largest UNDEVELOPED Cu-Ni-PGE The Largest UNDEVELOPED Cu-Ni-PGE Deposit on EarthDeposit on Earth
From Peterson, 2010
Duluth deposits are perceived as low grade. But compared to the source of most of the world’s copper - Porphyry Copper
Deposits...
…the Duluth Complex ores are HIGHER GRADE with MORE CONTAINED METAL than nearly all porphyry systems.
The largest copper ore deposits in the USA are on this diagram, and the Duluth Complex ores are much larger then all of them.