IMPLICATIONS OF GAS-LIQUID PHASE TRANSITIONS FOR ENDOGENIC ORIGIN OF HYDROCARBONS

dc.contributor.authorMalyshev A.I.
dc.date.accessioned2022-07-18T05:29:12Z
dc.date.available2022-07-18T05:29:12Z
dc.date.issued2004
dc.description.abstractBased on elementary molecular-chemical concepts, one can trace the evolution of the gaseous phase of an endogenic fluid at its temperature equilibrium with host rocks. As can be seen, the final result of this evolution consists in hydrocarbon formation within the hydrogen sulfide (point C) and carbon dioxide (point D) condensation zones.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13450083
dc.identifier.citationDoklady Earth Sciences, 2004, 399, 9, 1232-1235
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38224
dc.titleIMPLICATIONS OF GAS-LIQUID PHASE TRANSITIONS FOR ENDOGENIC ORIGIN OF HYDROCARBONS
dc.typeСтатья

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