HYBRIDIZATION OF MINGLING MAGMAS WITH DIFFERENT DENSITIES

dc.contributor.author	Albarede F.
dc.contributor.author	Grasset O.
dc.date.accessioned	2020-11-25T05:23:38Z
dc.date.available	2020-11-25T05:23:38Z
dc.date.issued	1995
dc.identifier	https://elibrary.ru/item.asp?id=658739
dc.identifier.citation	Earth and Planetary Science Letters, 1995, , 3, 559-560
dc.identifier.issn	0012-821X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19497
dc.description.abstract	It is usually assumed that chemical exchange between mafic enclaves considered as blobs of mafic liquids and their host silicic melt proceeds through static diffusion. However, the chemical boundary layer should keep the interior of magmatic enclaves nearly pristine, a feature which is not observed. The surface layer of a mafic blob falling in a more silicic melt is likely to be continuously folded in with the inner part. A numerical model shows that buoyancy-driven forced convection is an efficient way of enhancing the rate at which melt inclusions become hydrous and hybridized by the host melt.
dc.title	HYBRIDIZATION OF MINGLING MAGMAS WITH DIFFERENT DENSITIES
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.