Month: September 2018

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GEOLOGICAL, STRUCTURAL AND GEOCHEMICAL FEATURES GENERATION OF HYDROCARBONS OF THE SRIBNYANSKA DEPRESSION

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Geology & Geochemistry of Combustible Minerals No. 1-2 (174-175) 2018, 40-53.

Vitaliy GLON

Institute of Geological Sciences of National Academy of Sciences of Ukraine, Kyiv, е-mail: italiyglon@gmail.com

Abstract

Complex researches are conducted on the territory of the Sribnyanska depression. Systematic analysis of structural-thermal-atmogeochemical researches of oil and gas perspective objects of the Dnieper-Donetsk Rift was carried out. Interpretation and generalization of the received data was carried out. Criteria of oil and gas prospective formation complexes have been described. Based on the distribution of criteria of structural-thermal-atmogeochemical researches, prospects areas for the search of hydrocarbons within the limits of the Sribnyanska depression have been identified.

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Keywords

Dnieper-Donetsk Rift, Sribnyanska depression, oil and gas prospects, anomalies, hydrocarbons.

Referenses

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TWO HYPOTHESES – TWO APPROACHES TO SOLUTION OF THE PROBLEM OF OIL GENESIS

Home > Archive > No. 1-2 (174-175) 2018 > 28-39

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.

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Keywords

inorganic and organic synthesis, mantle, Pangea – 0, 1, 2, 3, Gondwana, Laurasia, rifting, mantle fluid-dynamic systems, depletion.

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