The article describes tectonics and the deep structure of the lithosphere in the eastern fragment of the Mongol-Okhotsk orogenic belt according to results of analysis of the geological and geophysical database. With account of palinspastic reconstructions, the model is developed to show the most probable paleogeodynamics of the lithosphere in the Mongol-Okhotsk orogenic belt and its heterochronous terrains.
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Shevchenkо et al. (2014) studied this question.
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