FIRST CLIACHITE AND FIND IN PACIFIC PELAGIC SEDIMENTS

dc.contributor.author	Arkhipova L.D.
dc.contributor.author	Galiy S.A.
dc.contributor.author	Korsakov O.D.
dc.contributor.author	Kruglyakov V.V.
dc.contributor.author	Marushkin A.I.
dc.date.accessioned	2020-04-15T06:25:19Z
dc.date.available	2020-04-15T06:25:19Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=30978450
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1987, 296, 5, 135-137
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16753
dc.description.abstract	Cliachite or alumogel (ALOOH + aq) is a gel-like, X-ray-amorphous aluminum hydroxide, and has so far been described only in bauxite and laterite, where it is mixed with boehmite, hydrargillite and diaspore and is primary relative to these minerals. It is assumed to form via coagulation of colloidal solutions of aluminum and by their conversion to a solid. The authors have discovered cliachite segregations in pelagic sediments of the Northeast Pacific Basin. They occur here very sporadically. Isolated cliachite grains were detected merely in 15 of the 600 sand-silt fractions examined, and only in one sample did cliachite account for as much as 38 percent of the silt fraction.
dc.title	FIRST CLIACHITE AND FIND IN PACIFIC PELAGIC SEDIMENTS
dc.type	Статья

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