SUBMICROSTRUCTURE OF TODOROKITE FROM THE OCEAN FLOOR

dc.contributor.author	Grigor'yeva T.N.
dc.contributor.author	Vasil'yeva A.I.
dc.date.accessioned	2020-04-16T07:05:03Z
dc.date.available	2020-04-16T07:05:03Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=31019922
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 301, 4, 135-137
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16840
dc.description.abstract	The authors have estimated the structural perfection (CSR and MD)2 of real crystals in specially selected suites of todorokite samples that were taken from two types of such crusts, differing in age, structure and mineral composition of their ore shells. It was found that these parameters tend to vary with the conditions of formation and type of paragenesis, and that there are broader opportunities for using X-ray methods to solve genetic problems. The fourth-component method was chosen from among the others to determine the submicroscopic structural parameters of todorokite because the latter has a specific X-ray diffraction pattern; the 9.6-angstrom reflection for the manganese minerals todorokite, buserite and asbolite is diagnostic Study results are discussed.
dc.title	SUBMICROSTRUCTURE OF TODOROKITE FROM THE OCEAN FLOOR
dc.type	Статья

Files in this item

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