Abstract
In the central part of the Altai-Sayan folded region (ASFR), intensive post-collisional continental magmatism of increased alkalinity has long been known. The products of this magmatism are widely distributed, both in the basal part of the Minusinsk basin section and in the smaller superimposed structures within their fold structures.
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Perfilova, O.Y., Sazonov, A.M., Makhlaev, M.L., Vorontsov, A.A. (2020). Igneous Rocks of the Kachinsk-Shumikhinsky Magmatic Area of Late Ordovician-Early Silurian Age (East Sayan). In: Ernst, R., Vrublevskii, V., Tishin, P. (eds) Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin. GeoGuide. Springer, Cham. https://doi.org/10.1007/978-3-030-29559-2_7
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