SPANISH HIGH-POTASSIUM MAGMAS AND EVIDENCE OF THEIR GENERATION DEPTH (AS INFERRED FROM THERMOBAROGEOCHEMICAL DATA)

dc.contributor.author	Solovova I.P.
dc.contributor.author	Kogarko L.N.
dc.contributor.author	Ryabchikov I.D.
dc.contributor.author	Naumov V.B.
dc.contributor.author	Girnis A.V.
dc.contributor.author	Kononkova N.N.
dc.contributor.author	Venturelli G.
dc.date.accessioned	2020-04-08T08:52:37Z
dc.date.available	2020-04-08T08:52:37Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30935948
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 100-103
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16390
dc.description.abstract	The ultrapotassic rocks of Spain have a number of features that relate them to diamond-bearing lamproites of Australia, although there also are some differences. Measurements of homogenization and resorption temperatures of daughter minerals in melt inclusions show that the subliquidus minerals here are olivine and chrome spine. Comparison of the Australian and Spanish lamproites shows that relatively shallow-depth processes were important in their formations. From our data, we conclude that high-potassium igneous rocks, geochemically similar to Spanish lamproites, have little diamond potential.
dc.title	SPANISH HIGH-POTASSIUM MAGMAS AND EVIDENCE OF THEIR GENERATION DEPTH (AS INFERRED FROM THERMOBAROGEOCHEMICAL DATA)
dc.type	Статья

Files in this item

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