GEOTHERMIC FIELD AND DEVELOPMENT OF THE STRUCTURE OF CONTINENTS

dc.contributor.author	Beloussov V.V.
dc.date.accessioned	2020-02-25T10:45:32Z
dc.date.available	2020-02-25T10:45:32Z
dc.date.issued	1985
dc.identifier	https://elibrary.ru/item.asp?id=30937459
dc.identifier.citation	JOURNAL OF GEODYNAMICS, 1985, 4, 1-4, 39-44
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16132
dc.description.abstract	Tectonic, magmatic and metamorphic processes combine into endogenous regimes. There is direct correlation between the degree of excitation of endogenous regimes and observed heat flow. There are grounds to suppose that all varieties of endogenous regimes, their distribution and their history depend on the heterogeneity in space and time of the Earth's thermal field.
dc.title	GEOTHERMIC FIELD AND DEVELOPMENT OF THE STRUCTURE OF CONTINENTS
dc.type	Статья

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