DETERMINING HEAT FLOWS AND RADIOGENIC HEAT GENERATION IN THE CRUST AND LITHOSPHERE BASED ON SEISMIC DATA AND SURFACE HEAT FLOWS

dc.contributor.author	Kronrod V.A.
dc.contributor.author	Kuskov O.L.
dc.date.accessioned	2024-10-23T07:16:01Z
dc.date.available	2024-10-23T07:16:01Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13512269
dc.identifier.citation	Geochemistry International, 2006, 44, 10, 1035-1040
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46162
dc.description.abstract	The balance of the Earth’s energy involves the generation of radiogenic, gravitational, chemical, and other types of energy and the heat loss from the Earth’s surface. In the quasi-stationary formulation, heat losses through the surface are equal to the sum of energy generated by all sources in the Earth’s interiors. The flow from the continental surface is estimated at 47–49 mW/m2. Estimates (accomplished by various researchers) of the mantle component of the heat flows range from 3 to 25 mW/m2.
dc.title	DETERMINING HEAT FLOWS AND RADIOGENIC HEAT GENERATION IN THE CRUST AND LITHOSPHERE BASED ON SEISMIC DATA AND SURFACE HEAT FLOWS
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906100089

Files in this item

Name: Kron_06.pdf

Size: 152.9Kb

Format: PDF