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

dc.contributor.author	Malyshev A.I.
dc.date.accessioned	2022-07-18T05:29:12Z
dc.date.available	2022-07-18T05:29:12Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13450083
dc.identifier.citation	Doklady Earth Sciences, 2004, 399, 9, 1232-1235
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38224
dc.description.abstract	Based 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.title	IMPLICATIONS OF GAS-LIQUID PHASE TRANSITIONS FOR ENDOGENIC ORIGIN OF HYDROCARBONS
dc.type	Статья

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