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Geology & Geochemistry of Combustible Minerals No. 3-4 (176-177) 2018, 28-39.
Orest STUPKA
Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, e-mail: igggk@mail.lviv.ua
Abstract
Origin of oil in great quantity took place in the history of the planet only once: in the Neogene, and there was no an analogy during last geological periods. This was connected with Post-Permian destruction of Gondwana. Destruction of this monolith massif, which 2/3 of the Pre-Cambrian sialic crust of Pangea which a thick (500–700 km) lithosphere was concentrated in, has led to formation of riftzones. They were characterized by the occurrence in the inner plate areas without subordination to the boundaries of lithospheric plates and not dependent on interaction between them. These zones have provided a deep drainage of the “initial” nondepleted lover mantle. It was just the lower mantle, but not the depleted upper one, that was a source of fluidal systems saturated with donators of chemical elements which are necessary for the synthesis of oil.
Keywords
inorganic and organic synthesis, mantle, Pangea – 0, 1, 2, 3, Gondwana, Laurasia, rifting, mantle fluid-dynamic systems, depletion.
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