Abstract
The results of 40Ar/39Ar dating of pseudotachylytes, first identified in the Paleoproterozoic zonally metamorphosed (greenschist to granulite facies) Ladoga complex of svecofennides, are presented. A wide age range of the formation of pseudotachylytes in the Riphean (1.59–1.31 Ga), presumably caused by the exhumation of deep rocks during the Svecofennian tectonogenesis and the subsequent orogenesis and riftogenesis in southeastern Fennoscandia, has been established.
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ACKNOWLEDGMENTS
We are grateful to Professor R.V. Veselovskii (Moscow State University; Schmidt Institute of Physics of the Earth, Russian Academy of Sciences) for assistance in the performance of this work and discussion of results.
Funding
This work was performed within the state assignments of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, and the Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, and was supported in part by the Russian Foundation for Basic Research, project no. 19–05–00256 (synmetamorphic structure formation in the sedimentary cover–basement system).
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Translated by D. Voroshchuk
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Morozov, Y.A., Yudin, D.S., Travin, A.V. et al. The First Discovery of Pseudotachylytes in the Paleoproterozoic Ladoga Zonal Metamorphosed Complex of Fennoscandia and Their 40Ar/39Ar Dating. Dokl. Earth Sc. 493, 485–489 (2020). https://doi.org/10.1134/S1028334X20070119
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DOI: https://doi.org/10.1134/S1028334X20070119