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Archean cratons are dominated by tonalite–trondhjemite–granodiorite (TTG) suites, the products of crustal differentiation that formed early continental crust. These rocks may have been primarily generated by partial melting of hydrated basaltic crust in a variety of settings including subduction zones or the deep lithosphere. Sources are mainly inferred from examination of TTGs alone, as potential source rocks are rarely exposed. In the southern Superior Province, Canada, the Kapuskasing Uplift exposes an important crustal cross-section with upper- to middle-crustal TTGs and lower-crustal metabasites, which show evidence of having produced trondhjemitic anatectic melt. Here, we test the hypothesis that these metabasites were the source of the Mesoarchean to Neoarchean TTGs in the Kapuskasing Uplift by combining phase equilibrium and melt trace element modelling with whole-rock and zircon Lu–Hf isotope analysis and geochronology (garnet Lu–Hf and zircon U–Pb) of metabasic samples. By comparison of the results with existing data from TTGs in the Kapuskasing Uplift, we determined that the metabasites are plausible source rocks for the TTGs. The Lu–Hf systematics of the metabasites and TTGs are the most robust evidence of a genetic connection. Modelling results support an increase in TTG source depth over time. New geochronological data constrain partial melting of metabasite and crystallization of anatectic melt between ca. 2685 Ma and ca. 2600 Ma, coeval with crystallization of only the youngest TTGs. Overall, these results indicate a complex history of intracrustal differentiation in the Kapuskasing Uplift, with partial melting of two isotopically distinct lower-crustal metabasic sources at different times and depths. [ABSTRACT FROM AUTHOR]

The Bancroft terrane and the associated Central Metasedimentary Belt boundary thrust zone represent the northern part of the Central Metasedimentary Belt (CMB) of the Canadian Grenville Province. Only a few direct pressure and temperature calculations based on phase equilibrium petrology methods exist in the central Bancroft terrane, and this study applies thermodynamic approaches such as garnet isopleth geothermobarometry to fill this gap and investigate the metamorphic history of the northern CMB. Four metapelitic rock samples were collected in the vicinity of the enigmatic Bancroft shear zone, which approximates the border between the Bancroft terrane and the Elzevir terrane to the south. Garnet isopleths for these samples only intersect if a certain amount of excess oxygen is added to the bulk rock composition corresponding to a [Fe.sup.3+]/F[e.sub.tot] ratio of 0.33-0.38. The northernmost sample records metamorphic peak conditions of approximately 1 GPa and 780 [degrees]C, whereas the southernmost sample, which is located in the Elzevir terrane, records a peak metamorphic pressure of approximately 0.9 GPa at a temperature of 520 [degrees]C. The latter result contradicts previous pressure estimates of the region and the proposed metamorphic field gradient but is based on a poorly constrained sample in terms of thermodynamic modeling. Hence, we conclude that the metamorphic field gradient in the northern CMB conceals two different P-T trajectories. Such a scenario is commonly observed in crustal thickening models and suggests that the cold upper plate (Elzevir terrane) was thrust over the warm lower plate (Bancroft terrane) in a northwesterly direction. Key words: Bancroft terrane, Central Metasedimentary Belt, Grenville Province, excess oxygen, thermodynamic modeling. Le terrane de Bancroft et la zone de chevauchement bordant la ceinture metasedimentaire centrale associee representent la partie nord de la ceinture metasedimentaire centrale (CMC) de la Province canadienne de Grenville. Seules quelques determinations directes de la pression et de la temperature basees sur des methodes petrologiques d'equilibre des phases existent pour la partie centrale du terrane de Bancroft, et la presente etude applique des approches thermodynamiques comme la geothermobarometrie basee sur les isoplethes de grenat pour combler cette lacune et examiner l'histoire metamorphique de la partie nord de la CMC. Quatre echantillons de metapelite ont ete preleves a proximite de l'enigmatique zone de cisaillement de Bancroft, qui marque l'emplacement approximatif de la limite entre le terrane de Bancroft et le terrane d'Elzevir au sud. Les isoplethes de grenat pour ces echantillons ne se croisent que si une certaine quantite d'oxygene excedentaire est ajoutee a la composition de la roche totale correspondant a un rapport [Fe.sup.3+]/F[e.sub.tot] de 0,33-0,38. L'echantillon preleve le plus au nord donne des conditions du pic du metamorphisme d'environ 1 GPa et 780 [degrees]C, alors que l'echantillon preleve le plus au sud, dans le terrane d'Elzevir, enregistre une pression metamorphique d'environ 0,9 GPa a une temperature de 520 [degrees]C. Ce dernier resultat est en contradiction avec des estimations passees de la pression pour la region et le gradient metamorphique de terrain propose, mais repose sur un echantillon dont le modele thermodynamique est mal contraint. Nous en concluons que le gradient metamorphique de terrain dans la partie nord de la CMC dissimule deux trajectoires P-T differentes, un scenario souvent observe dans des modeles d'epaississement crustal et qui indiquerait que la plaque superieure froide (terrane d'Elzevir) a ete charriee vers le nord-ouest sur la plaque inferieure chaude (terrane de Bancroft). Mots-cles : terrane de Bancroft, ceinture metasedimentaire centrale, Province de Grenville, exces d'oxygene, modelisation thermodynamique., Introduction The Canadian Grenville Province exposes the western roots of an ancient orogenic belt that surrounded the Laurentian and Baltic cratons, forming the supercontinent Rodinia around 1 Ga (e.g., Cawood [...]

Heat generated from the decay of K, Th, and U plays a fundamental role in the differentiation and stabilization of Earth's continental crust. This is particularly important in the construction of Archean cratons that form the nuclei of Earth's continents. The Kapuskasing uplift is a rare exposure of an Archean‐age crustal cross‐section that provides a snapshot of crustal melting, differentiation, and compositional stratification. We integrate field observations, whole‐rock compositions, thermodynamic equilibrium and accessory mineral modelling with heat production and latency time modelling to provide insights into the partitioning of heat‐producing elements between residue and melt during anatexis of metabasites as well as the resulting effects on metamorphic timescales and the production of tonalite–trondhjemite–granodiorite (TTG) suites. We model six metabasite compositions ranging from relatively fertile greenschist facies metabasites to melt‐depleted residual mafic (upper‐)amphibolites to granulites. Heat‐producing elements are modelled to be partitioned between melt and residue; the dominant minerals in the residue that host these elements are apatite, hornblende, K‐feldspar, and epidote. At 800–850°C epidote is no longer stable, and the melt fraction is predicted to contain roughly half of the heat production capacity for the system. Apatite and melt are expected to be the dominant repositories for Th and U during anatexis; zircon is predicted to be completely consumed by 850°C, whereas apatite persists to higher temperatures and allanite is expected only in minor modal abundances at high‐P, low‐T conditions. The partitioning of heat‐producing elements into relatively low‐density melt decreases the heat production of the residual system during anatexis. Due to their high density and affinity for U and Th, epidote and apatite retain heat production capacity in the residue during metabasite melting. Thermal latency modelling of metamorphism suggests that enriched metabasite compositions require 38–46 My to increase the temperature from ~650 to 850°C (solidus temperature to peak metamorphic temperature of the Kapuskasing uplift), whereas estimates are considerably shorter for depleted compositions (7–25 My). Four of the six samples modelled require 60–70 My to reach 1000°C from the solidus. Our modelling of heat‐producing element partitioning and predicted proportions of melt suggest that enriched basaltic compositions are the most reasonable source of TTG magmas and our heating time modelling indicates the mantle as an equal to dominant source of heat for metabasite anatexis compared with radiogenic heat production. [ABSTRACT FROM AUTHOR]

Tonalite-trondhjemite-granodiorite (TTG) suites are the dominant component of Earth's first continents, but their origins are debated. The trace element concentrations of these rocks are conventionally linked to their source depths and inferred geodynamic settings with the implicit assumption that TTG compositions are source-controlled. Alternatively, their variable compositions may be caused by fractional crystallization in TTG plutons after emplacement and less clearly linked to source depth. Most TTGs in Archean mid-crustal exposures are the dominant component of igneous gray gneiss complexes; the processes that influence the evolution of TTG magmas in this setting are poorly understood. We present a petrological-geochemical model that explains the coexistence of TTGs in the middle crust with low-pressure and high-pressure geochemical trends, irrespective of tectonic setting or depth of the TTG source. We propose that mid-crustal TTGs were long-lived crystal mushes with compositions controlled by the separation of early-crystallizing plagioclase and melt. Using phase equilibrium modeling, we demonstrate that a suite of TTGs from the southern Superior Province in Canada represents variably plagioclaserich and melt-rich fractions from a common parent magma. The behavior of plagioclase may have a strong influence on the geochemical trends of TTGs, including the degree of rare earth element fractionation. Our results suggest that trace element compositions of TTGs may not primarily reflect the depth of the source and cannot be used alone to infer Archean geodynamic settings. [ABSTRACT FROM AUTHOR]