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Igneous Stratigraphy of the

Layered Series at Duluth

Type Intrusion of the Duluth Complex

James D. Miller

Department of Geological Sciences

and Precambrian Research Center

University of Minnesota Duluth

This trip guide is a modified from a guidebook entitled Field Guide to the Geology and Mineralization of Mafic Layered Intrusions of the Duluth and Beaver Bay Complexes, Northeastern Minnesota (Miller and Severson, 2009). The guidebook was developed for a field trip associated with the Precambrian Research Center Professional Workshop on Field, Petrographic and Mineralization Characteristics of Mafic Layered Intrusions held October 4-10, 2009

Geology and PGE Mineralization of the Layered Series at Duluth

The well-exposed gabbroic rocks forming the escarpment above the city of Duluth have long been recognized as the type section of the Duluth Complex. While early surveys recognized the presence of two distinct rock types in the Duluth area (Winchell, 1899), Grout was the first to interpret the layered gabbros as a product of convection and magma differentiation (Grout, 1918a-e). Taylor (1964) produced the first detailed-scale (1:24,000) geologic map of the complex in the Duluth area and defined the main distinctions between the layered and anorthositic series. Moreover, based on field, petrographic, and very limited geochemical data, Taylor recognized basic similarities between the layered series at Duluth and the Skaergaard intrusion, which Wager and Deer (1939) had established as the classic example of a mafic intrusion formed by closed-system fractional crystallization of a tholeiitic magma. More recently, detailed mapping in the Duluth area has delineated much more about the structure and cumulate stratigraphy of the layered series (Miller and Green, 2008a & b; Green and Miller, 2008). The petrology of the layered series was summarized by Miller and Ripley (1996) and Miller and Severson (2002).

The Layered Series at Duluth (DLS) is a well-differentiated, 3- to 4.5-km-thick, east-dipping sheet-like mafic layered intrusion that is the southernmost intrusion of the Duluth Complex. Exposure is very good along the 600'-high escarpment above Lake Superior and the St. Louis River estuary, but is spotty inland. Aeromagnetic data show that the DLS has a north-south strike length of about 60 kilometers long and eventually pinches out into the Boulder Lake intrusion. The hanging wall of the DLS consists of olivine gabbroic and troctolitic anorthosite of the anorthositic series, which according to U-Pb dating was emplaced just prior to DLS intrusion at 1099 Ma (Paces and Miller, 1993). The footwall of the DLS at its southern end is reversed polarity lavas of the Ely's Peak basalts (Fig. 1-1). Layering and foliation in the DLS, which dip 20º-40º to the east, and modeling of aeromagnetic and gravity data indicate that the basal contact is not conformable with shallow-dipping (~15°) Keweenawan basalt flows in the footwall, but instead dips at a greater than 35° angle (Miller and Green, 2008b). Aeromagnetic data further imply that the basalt is cut out by the DLS to the north, whereupon the footwall becomes graywacke and slates of the Thomson Formation.

Figure 1-1. Geology of the Duluth Complex at Duluth showing the field trip stops.

The DLS is divided into five major zones based on dominant rock type (Fig. 1-1). The basal contact zone is composed of coarse-grained, taxitic olivine gabbro and augite troctolite (Stop 1). The lowermost cumulate sequence is the troctolite zone (Stops 1, 2A & 2B). It is 1 to 2 kilometers thick, consists mostly of homogenenous foliated troctolitic (PO) cumulates, and locally displays modal and textural layering, especially in its lower third. The cyclic zone (Stops 3, 4, & 5) forms the medial section of the DLS and is characterized by cyclical variations in cumulus mineralogy between troctolitic and gabbroic (PCFO) cumulates (Fig. 1-4). The persistent occurrence of gabbroic cumulates defines the gabbro zone. Gabbroic cumulates, in turn, grade upward into unlaminated (noncumulate) apatitic quartz ferromonzodiorite, which composes most of the upper contact zone (Stop 6). This quartz ferromonzodiorite complexly mixes with a fine-grained biotitic ilmenite ferrodiorite, which ultimately forms a ';chilled'; contact with anorthositic series rocks (Stop 7). A body of melanogranophyre that irregularly cuts through the anorthositic series probably represents the uppermost differentiate of the DLS (Stop 8). This igneous stratigraphy is complimented by cryptic layering of cumulus mineral compositions (Fig. 1-2) and together these imply the DLS generally formed by bottom-up fractional crystallization of a
moderately evolved, olivine tholeiitic parent magma.

Figure 1-2. Igneous stratigraphy and cryptic variation of olivine, pyroxene and plagioclase composition through the Layered Series at Duluth. mg# values of olivine and pyroxene and An content of plagioclase are based on multiple microprobe analyses (error bars indicate one standard deviation). From Miller and Severson, 2002, Figure 6.8.

Although the DLS is overall,

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