DIAMETER AND FORMATION TIME OF PLUME HEAD AT THE BASE OF REFRACTORY LITHOSPHERIC LAYER

dc.contributor.author	Dobretsov N.L.
dc.contributor.author	Kirdyashkin A.A.
dc.contributor.author	Kirdyashkin A.G.
dc.date.accessioned	2024-10-27T02:28:50Z
dc.date.available	2024-10-27T02:28:50Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518689
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 56-60
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46279
dc.description.abstract	Estimation of the growth time and dimension of plume head (PH) ascent from the deep mantle toward the lithosphere is an important problem of geodynamics, towards the solution of which an active search is presently being carried out. An experimental and theoretical model of the plume that spreads at the lithosphere base is presented. This model envisages the ascent of a purely chemical plume driven by a density difference between the low-viscous plume material and the high-viscous ambient massif.
dc.subject	plume head
dc.title	DIAMETER AND FORMATION TIME OF PLUME HEAD AT THE BASE OF REFRACTORY LITHOSPHERIC LAYER
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010144

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