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JIM MILLER RESEARCH CENTER DEPT. OF GEOLOGICAL SCIENCES UNIVERSITY OF DULUTH

Minnesota Ground Water Association Spring Meeting May 6, 2010 Talk Outline • History of Geologic Mapping • Evolution of the Midcontinent Rift •Geology & Genesis of the •Cu-Ni-PGE Mineralization Stillwater Complex, Montana

Skaergaard, East Greenland

Sudbury Complex, Second Ontario DuluthDuluth Largest Complex Great Complex Dyke, Zimbabwe Complex in Bushveld Complex, the World South Africa

circa 1872 Minnesota Geological Survey 1872 - 1900

N.H. Winchell The Grout and

F.F. Grout Schwartz Era 1911-1958 G.M. Schwartz

Saganaga Lake, Aug. 1922

“Chicken-track” Reconnaissance Mapping

Sonju Lake area geology 1939 Grout, 1918 Geology of Northeast Minnesota

circa 1932 The Quadrangle Mapping Era 1961 - 1982 P.K. Sims, MGS Director 1961-1973 Matt Walton, MGS Director, 1973-1987 J.C. Green – North Shore Volcanics P.W. Weiblen - Bald Eagle Int, Long Is. Lk. W.C. Phinney - NW Duluth Complex D.M. Davidson Jr. - E Duluth Complex B. Bonnichsen - S Duluth Complex, Babbitt Ph.D. Theses R.B. Taylor – Duluth area H.D. Hathan – Gunflint Trail area E.A. Mathez – Logan Sills M.G. Mudrey – Pigeon Point R.W. Cooper – Babbitt/Harris Lake area M.P. Foose – Harris Lake area MGS Misc. Map M-1 M.S. Theses 1964, R.B. Taylor N.W. Jones – Hovland Db, Logan Sills J.A. Kilburg – Ely’s Peak J.R. Burnell – R.J. Stevenson – Sonju Lake Intrusion N.M. Pope – Silver Cliff/Lafayette Bluff John Green Bill Phinney Paul Weiblen

Gooseberry Falls, 1996

Gabbro Lake 15’ Quadrangle MGS Miscellaneous Map M-2 Green, Phinney, & Weiblen, 1966 massive sulfide, basal DC Phinney

Nathan/Mathez

Bonnichsen

Davidson Two Harbors Sheet J.C. Green 1982 Aeromagnetic Survey of NE Minnesota 1979-1982

First Vertical Derivative of Aeromagnetic Data Shallow Drilling Program 1993-1995

Well Exposed

Poor Exposure

No Exposure Compilation of the Geologic Picture 2001 MGS Miscellaneous Map M-119, 2001

MGS Report of Investigations 58 2002 Geologic Mapping since 2001 The need for an update ______

THE MIDCONTINENT RIFT ______An attempt at continental rifting 1.1 billion years ago A. Rift Magmatism

Basalt The Evolution of Gabbro Flows the Midcontinent

Crust Rift Mantle 1,109-1,086 Ma Mantle Plume

B. Sediment Infilling Sandstone

1,090-900 Ma

C. Compression

1,000-900 Ma GLIMPCE Seismic Line A from Trehu et al., 1994 Bimodal Magmatism of the Midcontinent Rift From Miller & Vervoort (1996)

Litho/ of the North Shore Volcanic Group

From Davis and Green (1997) THE DULUTH COMPLEX Felsic Series 1109-1106 Ma (Vervoort et al., 2007) Poplar Lake Intrusion Crocodile Lake Intrusion

Early Gabbro Series 1107 Ma Paces & Miller, 1993 Davis and Green, 1997 Anorthositic Series troctolitic (TA)

poikilitic olivine anorthosite (poA) 1099 Ma (Paces & Miller, 1993)

olivine leucogabbro (oLG)

mgTA gabbroic anorthosite (GA)

cgTA

1099 Ma (Paces & Miller, 1993) Layered Series

CUMULUS STRATIGRAPHY IN LS INTRUSIONS Pl+Cpx+Ox+Ol+Ap+Gp

layered troctolite OLI – Osier Lake Intrusion Pl+Cpx+Ox+/-Ol DLS – Layered Series at Duluth BEI – Bald Eagle Intrusion WLI – Wilder Lake Intrusion GLI – Greenwood Lake Intrusion BLI – Boulder Lake Intrusion Pl+Ol WMI – Western Margin Intrusion SKI – South Kawishiwi Intrusion TI – Tuscarora Intrusion L1 – Lake One Intrusion Ol PRI – Partridge River Intrusion X-bedded olivine gabbro Beaver Bay Complex 1096 Ma (Paces & Miller, 1993)

Topography and Geology in the Tettegouche State Park Area

Anorthosite Inclusions in the Beaver River Diabase Origin of Anorthositic Rocks of the Duluth and Beaver Bay Complexes Contact Zone Cu-Ni-PGE Sulfide Deposits of the Duluth Complex

Average Grades Cu – 0.6% Ni - 0.2% Co – 0.005% Pd+Pt+Au – 500-1000 ppb Creation of the Cu-Ni-PGE Sulfide Deposits of the Duluth Complex

Cu S Ni S Co

Pd + Pt Au Dominant Mineralogy of Magmatic Cu-Ni Sulfide Deposits

Pyrrhotite – FeS1-x

Chalcopyrite - CuFeS2

Pentlandite - (Fe,Ni)9S8

Bornite - Cu5FeS4

Talnakhite – Cu9(Fe,Ni)8S16

Chalcocite - Cu2S Cobaltite - CoAsS Mineralization Model for the Basal Intrusions of the Duluth Complex Styles of Mineralization after Peterson (2001) • Open (early) – vertically extensive (> 450 meters) – low - mod Cu-Ni and very low Au+PGE – Cu-Ni grades typically increase towards the basal contact • Confined (late) – vertically restricted (< 150 meters) – mod - high Cu-Ni and mod to high Au+PGE – Cu-Ni grades typically are the highest near the top of the mineralized zone Spruce Road, Open Style Maturi Deposit, Confined Style

Current Exploration Activity Polymet –Northmet Teck American –Mesaba Franconia – Birch Lake, Maturi, Spruce Rd Duluth Metals – Nokomis, Dunka Pit Encampment– South Filson Cr. A World Class Ore Deposit That Someday Will Be Mined

(Eckstrand and Hulbert, 2007)