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Geochemical and Sr–Nd Isotope Systematics of the Late Permian–Early Triassic Traps from the Kuznetsk Basin: Magma Sources and Correlation with the Noril’sk Region Volcanics

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Abstract

The study provides whole-rock geochemical and Rb–Sr and Sm–Nd isotope examinations of Permian–Triassic volcanics (basalts, basaltic andesites) and sills (trachydolerites, monzodiorites) from the Kuznetsk Basin, which is part of the Siberian Large Igneous Province. It is shown that the volcanic section of the Kuznetsk Basin consists of the Lower (I and II units: TiO2 = 1.6–1.9 wt %, Gd/Yb = 2.0–2.1) and Upper (III–VIII units: TiO2 = 1.4–1.8 wt %, Gd/Yb = 1.7–1.9) sequences. The Mayzass sill is geochemically correlated with the Unit II basaltic andesite of the Lower Sequence, and the Syrkashev sill is geochemically akin to the Upper Sequence. The Kuznetsk traps originated from the partial melting of a Sr–Nd isotopically heterogeneous subduction-modified lithospheric mantle. They are geochemically comparable to low-Ti basalts of the low–middle Nadezhdinsky suite from the Noril’sk region, but differ in Sr–Nd isotope composition. The Sr–Nd isotope signatures of non-contaminated lavas and rocks of the Syrkashev sill (εNd(T) = (+4.6)–(+2.4), (87Sr/86Sr)T = 0.7047–0.7054) are inherited from the ancient lithospheric mantle and do not represent the contribution of the Siberian plume. The Mayzass sill rocks (εNd(T) = (+2.2)–(+2.1); (87Sr/86Sr)T = 0.7055–0.7063) are derived from a parental melt contaminated with crustal carbonates.

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ACKNOWLEDGMENTS

The author gratefully acknowledges A.V. Nastavko for  his immense assistance in sampling, as well as Dr.  N.N. Kruk and anonymous reviewers for their helpful remarks during the article’s preparation.

Funding

This study is done on state assignment of IGM SB RAS (122041400237-8).

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  1. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, 630090, Novosibirsk, Russia

    T. V. Svetlitskaya

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Svetlitskaya, T.V. Geochemical and Sr–Nd Isotope Systematics of the Late Permian–Early Triassic Traps from the Kuznetsk Basin: Magma Sources and Correlation with the Noril’sk Region Volcanics. Dokl. Earth Sc. 510, 400–410 (2023). https://doi.org/10.1134/S1028334X23600263

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