For the first time, the diagram of the average speed variations of movement of lithospheric plates (LPs) in the Fanerozoic has been built, where the most important world stratigraphic levels of formation of domanik-like (potentially oil-source) sediments, which are enriched with organic matter, are shown. An analysis of the diagram has revealed substantial differences in the rhythmic of LPs movement and features of spreading the domanik-like sediments in the Paleozoic and Mesocenozoic megacycles.

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