Implications for the origins of Eoarchean ultramafic rocks of the North Atlantic Craton: a study of the Tussaap Ultramafic complex, Itsaq Gneiss complex, southern West Greenland

Contributions to Mineralogy and Petrology volume 174, Article number: 96 (2019) Cite this article

Abstract

Ultramafic rocks found within the ~ 3.81 Ga Itsaq Gneiss Complex (IGC) have some mantle-like geochemical characteristics that have led to them being used to directly constrain the nature of the Eoarchean mantle. The discrimination of mantle peridotites that are the residues of partial melting, from cumulate peridotites generated by crystal accumulation from mantle-derived magmas can be difficult in ancient, altered ultramafic rocks whose field relations have been obscured by multiple tectonic episodes. Hence it is important to scrutinize significant individual occurrences of Eoarchean ultramafic rocks in some detail prior to using them to constrain the nature of Earth’s early mantle. Here we present mineral chemistry, whole rock major-, trace-, and platinum-group-element abundances, and Re–Os isotope compositions of a previously unstudied large ultramafic enclave in the IGC—the Tussaap Ultramafic Complex (TUC)—with the aim of documenting its origin. High FeO contents of up to 15.5 wt% and correlations between MgO and Os provide strong evidence that the TUC evolved through fractional crystallization rather than partial melt extraction. In addition, co-variations of major elements in the TUC lithologies can be modeled via fractional crystallization of picritic basalts using MELTS. Later alteration and metasomatism of these ultramafic rocks has largely overprinted primary mineral chemistry and resulted in a redistribution of light rare earth elements, rendering these tools ineffective for ascertaining the origin of the TUC or quantifying some of the petrogenetic processes that formed the body. In addition, it is clear that many geochemical features used to identify residual mantle peridotites can also be produced by cumulate or alteration processes, such as some variations in olivine and chromite chemistry, whole rock Al/Si vs Mg/Si systematics, and trace and platinum group element patterns. Finally, combined discrimination diagrams for high field strength elements and moderately high 187Os/188Os ratios suggest the parental melt of the TUC partially assimilated basaltic crust prior to precipitating the TUC cumulates. As such, these rocks represent a variably obscured record of Eoarchean crystal fractionation from mantle-derived melts. Despite not being prima facie mantle rocks, it is possible that such early formed ultramafic cumulates in nascent continents found their way into the later-stabilized roots of Archean cratons, helping to explain the high compositional variability of cratonic peridotites.

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Modified from Nutman et al. (2002)

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Acknowledgements

This work was funded by a Canada Excellence Research Chair award to Pearson and a Carlsberg Foundation fellowship (CF18-0090) to Szilas.

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Affiliations

  1. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada

    T. McIntyre & D. G. Pearson

  2. Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, 1350, Copenhagen K, Denmark

    K. Szilas

  3. Faculty of Geosciences and Civil Engineering, Institute of Science and Engineering, Kanazawa University, Kanazawa, Ishikawa, 920-1192, Japan

    T. Morishita

  4. Lamont-Doherty Earth Observatory, Columbia University, New York, NY, 10027, USA

    T. Morishita

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  1. T. McIntyre
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  2. D. G. Pearson
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  3. K. Szilas
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  4. T. Morishita
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Correspondence to T. McIntyre.

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McIntyre, T., Pearson, D.G., Szilas, K. et al. Implications for the origins of Eoarchean ultramafic rocks of the North Atlantic Craton: a study of the Tussaap Ultramafic complex, Itsaq Gneiss complex, southern West Greenland. Contrib Mineral Petrol 174, 96 (2019). https://doi.org/10.1007/s00410-019-1628-9

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Keywords

  • Eoarchean
  • Itsaq gneiss complex
  • Ultramafic cumulates
  • Platinum group elements
  • Re–Os isotopes