THE ORIGIN OF A HELIUM ISOTOPE ANOMALY IN THE NORTH OF THE MOUNT ELBRUS REGION

dc.contributor.author	Yakovlev L.E.
dc.contributor.author	Polyak B.G.
dc.date.accessioned	2021-01-01T09:12:24Z
dc.date.available	2021-01-01T09:12:24Z
dc.date.issued	1998
dc.identifier	https://elibrary.ru/item.asp?id=20946033
dc.identifier.citation	Volcanology & Seismology, 1998, , 6, 769-783
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22021
dc.description.abstract	This study elucidated the source of mantle helium rising to underground fluids in the zone of the recent magmatic activity in the northern Caucasus and the adjacent part of the Scythian Plate. It is shown by way of numerical hydrodynamic modeling that the helium observed in the fluids of the Mount Elbrus and Stavropol Arch regions rises not only through the central feeder of Elbrus Volcano but is also removed from deep-seated magmatic bodies containing mantle helium, which are more widespread than the surface products of magmatic activity.
dc.title	THE ORIGIN OF A HELIUM ISOTOPE ANOMALY IN THE NORTH OF THE MOUNT ELBRUS REGION
dc.type	Статья

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