RATE-CONTROLLED CALCIUM ISOTOPE FRACTIONATION IN SYNTHETIC CALCITE

dc.contributor.author	Lemarchand D.
dc.contributor.author	Wasserburg G.J.
dc.contributor.author	Papanastassiou D.A.
dc.date.accessioned	2022-03-19T11:05:23Z
dc.date.available	2022-03-19T11:05:23Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=12090422
dc.identifier.citation	Geochimica et Cosmochimica Acta, 2004, 68, 22, 4665-4678
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36445
dc.description.abstract	Calcium isotopic variations in carbonates, both marine organisms and inorganic systems, have recently been interpreted as a possible seawater temperature recorder [1,2]. In order to understand the behavior of calcium isotopes during precipitation of Ca-carbonate, synthetic calcite growth experiments were carried out at constant temperature and under various pH and alkalinity conditions.
dc.subject	calcite
dc.title	RATE-CONTROLLED CALCIUM ISOTOPE FRACTIONATION IN SYNTHETIC CALCITE
dc.type	Статья

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