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Geochronological analysis dates gabbrodolerites in Belarus, indicating deformation stages in geological history.
This work report on dating of the basic rocks of the “Big Dike” located in the south-eastern part of the crystalline basement of Belarus. U–Pb (ID-TIMS) geochronological studies of baddeleyite have established that the age of gabbrodolerites of the dike is 1788 ± 4 Ma, corresponding to the final events of the Subbotka-Moshorin deformation stage (1788–1792 Ma).
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Burmistrov et al. (2026) studied this question.
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