| Popis: |
A reaction for synthesis of hydrocarbons is considered in terms of a conceptual aqua-complex [2SiO3-OH2-Mn+2Mm+Oc 4] (n=1, 2; m≥3, O’-volatiles). Structural and chemical rearrangements are catalyzed within clay medium. Catalytic reactions are triggered by energy disequilibria in mineral systems caused by strain from the burial and compaction of sediments and by rock deformations during which C substitutes for Si in argillaceous rocks. Organic matter reduces C, which participates in the synthesis of hydrocarbon products. At present, this reaction is taking place in the bottom sediments of the Solenoe Lake (Kulunda steppe) located within one of several tectonic zones that parallel the main orogenic belt of the Altai. Geologic evidence and results of complex study of the bottom sediments support the relevancy of the proposed reaction mechanism, which combines “organic” and “inorganic” viewpoints on the origin of oil and gas. |
