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Evidence for the amalgamation of Archean oceanic and continental blocks to form the Beartooth Plateau

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Part of the book series: Proceedings of the International Conferences on Basement Tectonics ((ICBT,volume 2))

Abstract

The structure and age of the lithospere in the western Beartooth Plateau was investigated by geochemical study of Cretaeous igneous rocks derived from the deep crust and the lithospheric mantle and by study of exposed basement rocks. This study shows that the upper crust is dominated by ≈ 2740 Ma granitoids, similar to those widespread in the Beartooth Mountains. These have inclusions of supracrustal amphibolites and metasediments. Sm-Nd and Pb-Pb isotopic systematics of these rocks indicate that their protoliths were separated from the mantle only a few hundred million years prior to 2700 Ma, and no evidence of early Archean crust was found.

Cretaeous granitoids were derived from ≈ 3300 Ma deep crust with relatively low 87Sr/86Sr, 206Pb/204Pb, and εNd.This crust is believed to have been similar to exposed amphibolites. Trace-element and isotopic considerations show, however, that the source region contained little felsic material (granitoids or metapelites) and was dominated by amphibolites. The amphibolites and source regions of the granitoids had negative Ce-anomalies, indicating that these rocks has passed through a weathering cycle. Protoliths may have formed as mafic-intermediate lavas in an oceanic environment with little emergent land. The present-day upper crust may have formed when this terrane was closer to the continent or was more evolved.

The mantle in the area records an early Archean event and a Proterozioc event. These produced LILE-rich mantle with low Rb/Sr, Sm/Nd, and U/Pb that developed unusual isotopic compositions. Some Cretaceous magmas were derived from these sources.

The lithosphere structure dictates a history separate from the early Archean continent of the eastern Beartooth Mountains. I propose that the western Beartooth Plateau developed in an oceanic environment prior to ≈ 2800 Ma and was accreted to the eastern plateau during subduction at 2740–2790 Ma. The two terranes were amalgamated by ≈ 2740 Ma, as a simultaneous magmatic event affected both at that time.

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© 1992 Springer Science+Business Media Dordrecht

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Meen, J.K. (1992). Evidence for the amalgamation of Archean oceanic and continental blocks to form the Beartooth Plateau. In: Bartholomew, M.J., Hyndman, D.W., Mogk, D.W., Mason, R. (eds) Basement Tectonics 8. Proceedings of the International Conferences on Basement Tectonics, vol 2. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1614-5_20

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  • DOI: https://doi.org/10.1007/978-94-011-1614-5_20

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-4703-6

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