OXYGEN ISOTOPE STUDIES OF CARBONACEOUS CHONDRITES - A SURVEY

dc.contributor.author	Clayton R.N.
dc.contributor.author	Mayeda T.K.
dc.date.accessioned	2021-01-09T04:56:48Z
dc.date.available	2021-01-09T04:56:48Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=149022
dc.identifier.citation	Geochimica et Cosmochimica Acta, 1999, , 13, 2089-2104
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22444
dc.description.abstract	The carbonaceous chondrites display the widest range of oxygen isotopic composition of any meteorite group, as a consequence of the interaction of primordial isotopic reservoirs in the solar nebula. These isotopic variations can be used to identify the reservoirs and to determine conditions and loci of their interactions. We present a comprehensive set of whole-rock analyses of CV, CO, CK, CM, CR, CH, and CI chondrites, as well as selected components of some of these meteorites. A simple model is developed which describes the isotopic behavior during parent-body aqueous alteration processes. The process of thermal dehydration also produces a recognizable effect in the oxygen isotopic composition.
dc.title	OXYGEN ISOTOPE STUDIES OF CARBONACEOUS CHONDRITES - A SURVEY
dc.type	Статья

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