Precambrian Geology of the Lake Superior Region THE MAKING OF LAURENTIA Jim Miller University of Minnesota Duluth The Geologic Record in Minnesota LAURENTIA KENORALAND Precambrian Geology of Minnesota Direct Evidence: OUTCROP More Direct Evidence: DRILL CORE Image from Dale Setterholm, MGS Location of core hole Drill core 1st vertical derivative of aeromagnetic data Drill hole locations provided by Minnesota Department of Natural Resources, Division of Lands and Minerals, Hibbing 2002 Indirect Evidence: GEOPHYSICAL DATA Supporting Evidence: GEOCHRONOLOGY AND GEOCHEMISTRY Geologic Paradigms and Principles Terrane 1: The Minnesota River Valley Gneiss Terrane >3.0 Ga THE MINNESOTA RIVER VALLEY GRANITIC GNEISS Early Continent Formation Terrane 2: The Superior Province (GraniteGreenstone Terrane) 2.7-2.5 Ga GREENSTONE Metamorphosed Basalt Pillowed Structures indicative of submarine eruption SEDIMENTARY ROCKS BANDED IRON FORMATION GRAYWACKE GRANITE BATHOLITHS Partially-melted Crust (~ 2.6 Ga) The Superior Province Multiple Accreted Terranes TECTONIC MODEL FOR THE SUPERIOR PROVINCE Accretion of Island Arcs, Oceanic Plateaus, and Protocontinents SUPERIOR PROVINCE A major episode of continental growth creating KENORALAND, the core of North America Kenoraland Terrane 3: The Penokean (and Yavapi and Mazatzal) Orogen 1.9-1.6 Ga Making Laurentia MESABI-TYPE IRON FORMATION Geologic Marker of a Major Evolutionary Event STROMATOLITES (Fossilized Algal Mats) A Key to the Origin of Mesabi-type Iron Formation Mary Ellen Mine Shark Bay, Australia LTV Mine The 1.85 Ga Sudbury Impact The First Major Extinction Event ?? Penokean Orogeny 1.85 Ga Thomson Dam Eveleth St. Cloud Penokean Mountains (1.85 -1.75 Ga) DENUDATION OF A MOUNTAIN BELT SIOUX QUARTZITE and Related 1.7 Ga Mature Sandstones Flambeau Rib Mtn Sioux Baraboo The Amazing Shrinking Penokean (From Holm et al., 2008) NICE (Northern Interior Continental Evolution) Working Group: R. Anderson, T. Boerboom,W. Cannon, V. Chandler, D. Holm, M. Jirsa, J. Miller, D. Schneider, K. Schulz, W.R. Van Schmus, and L. Woodruff. GRENVILLE OROGENY 1150-950 Ma Adding Laurentia to the Supercontinent: Rodinia Terrane 4: The Midcontinent Rift 1.1 Ga An Attempt at Unmaking Laurentia Initiation of the MCR by the impact of a starting mantle plume A. Rift Magmatism Basalt Flows Gabbro Crust Mantle The Evolution of The Midcontinent Rift 1,109-1,086 Ma Mantle Plume B. Sediment Infilling Sandstone 1,090-900 Ma C. Compression 1,000-900 Ma Origin of MCR Igneous Rocks BASALT – The Rock of Oceanic Crust NORTH SHORE Continental Flood Basalts ICELAND HAWAII Massive Basalt Amygdaloidal Basalt AGATES Gemstone of Minnesota Formation of Lake Superior Agates High Falls on the Baptism River Shovel Point RHYOLITE The other volcanic rock type Palisade Head INTRUSIVE IGNEOUS ROCKS Gabbro Magmas trapped in the Crust Duluth Complex Layered Gabbro Beaver Bay Complex Granite SEDIMENTARY ROCKS of the Midcontinent Rift Freda Sandstone Interflow Conglomerate LATE-STAGE FAULTING The Douglas Fault at Amnicon Falls State Park Basalt Sandstone Why isn’t Duluth a Sea-side Resort? FINALLY, THE STABLE CONTINENTAL INTERIOR OF NORTH AMERICA The Precambrian Research Center at UMD