Abstract
The accretion of the Wyoming, Hearne, and Superior Provinces to form the Archean core of western Laurentia occurred rapidly in the Paleoproterozoic. Missing from Hoffman’s (1988) original rapid aggregation model was the Medicine Hat block (MHB). The MHB is a structurally distinct, complex block of Precambrian crystalline crust located between the Archean Wyoming Craton and the Archean Hearne Province and overlain by an extensive Phanerozoic cover. It is distinguished on the basis of geophysical evidence and limited geochemical data from crustal xenoliths and drill core. New U-Pb ages and Lu-Hf data from zircons reveal protolith crystallization ages from 2.50 to 3.28 Ga, magmatism/metamorphism at 1.76 to 1.81 Ga, and εHfT values from −23.3 to 8.5 in the Archean and Proterozoic rocks of the MHB. These data suggest that the MHB played a pivotal role in the complex assembly of western Laurentia in the Paleoproterozoic as a conjugate or extension to the Montana Metasedimentary Terrane (MMT) of the northwestern Wyoming Province. This MMT–MHB connection likely existed in the Mesoarchean, but it was broken sometime during the earliest Paleoproterozoic with the formation and closure of a small ocean basin. Closure of the ocean led to formation of the Little Belt arc along the southern margin of the MHB beginning at approximately 1.9 Ga. The MHB and MMT re-joined at this time as they amalgamated into the supercontinent Laurentia during the Great Falls orogeny (1.7–1.9 Ga), which formed the Great Falls tectonic zone (GFTZ). The GFTZ developed in the same timeframe as the better-known Trans-Hudson orogen to the east that marks the merger of the Wyoming, Hearne, and Superior Provinces, which along with the MHB, formed the Archean core of western Laurentia.
Highlights
The Precambrian Medicine Hat Block (MHB) lies south of the Archean Hearne Province (Figure 1), and it was originally defined by structural features in overlying Paleozoic sedimentary rocks [1] and subsequently by potential field and seismic surveys [2,3]
The Great Falls tectonic zone (GFTZ) developed in the same timeframe as the better-known Trans-Hudson orogen to the east that marks the merger of the Wyoming, Hearne, and Superior Provinces, which along with the MHB, formed the Archean core of western Laurentia
The MHB and Metasedimentary Terrane (MMT) re-joined at this time as they amalgamated into the supercontinent Laurentia during the Great Falls orogeny (1.7–1.9 Ga), which formed the GFTZ [1,28,56,57,58,59]
Summary
The Precambrian Medicine Hat Block (MHB) lies south of the Archean Hearne Province (Figure 1), and it was originally defined by structural features in overlying Paleozoic sedimentary rocks [1] and subsequently by potential field and seismic surveys [2,3]. The xenoliths are from Eocene minettes of the Sweetgrass Hills area of the Montana alkali province (MAP) located within southern Alberta and northern Montana (Figure 1; [6]). These alkaline volcanic-entrained xenoliths provide a unique opportunity to study the age and history of the enigmatic continental crust of the northwestern MHB (e.g., [5,7]) and the buried southern (Alberta) part of the western
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