SOLID SOLUTIONS WITH ENERGETICALLY NONEQUIVALENT SUBLATTICES AS SOURCE OF INFORMATION ON RATE OF POSTCRYSTALLIZATION COOLING OF MINERALS

dc.contributor.author	Akimov V.V.
dc.contributor.author	Abramovich M.G.
dc.date.accessioned	2020-04-10T02:18:07Z
dc.date.available	2020-04-10T02:18:07Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30954465
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 302, 5, 249-251
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16478
dc.description.abstract	The distribution of atoms in lattices of minerals such as alkali feldspars or orthopyroxenes have long been used to estimate the temperature of natural processes. We describe an approach to determining the kinetics of postcrystallization colling of minerals based on evaluation of the time-dependent relations. As an example we consider triclinic albite with one ordering parameter. However, our method can also be applied to crystals with several ordering parameters. Our approach allows one to employ data on mineral crystals with energetically nonequivalent positions in the lattice as 'geospeedometers' and to introduce corrections to the kinetics of the rock cooling in estimating the temperatures of mineral genesis.
dc.title	SOLID SOLUTIONS WITH ENERGETICALLY NONEQUIVALENT SUBLATTICES AS SOURCE OF INFORMATION ON RATE OF POSTCRYSTALLIZATION COOLING OF MINERALS
dc.type	Статья

Files in this item

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