LEAD AND STRONTIUM ISOTOPES AS MONITORS OF EXPERIMENTAL GRANITOID MINERAL DISSOLUTION

dc.contributor.author	Erel Y.
dc.contributor.author	Blum J.D.
dc.contributor.author	Roueff E.
dc.contributor.author	Ganor J.
dc.date.accessioned	2022-03-19T11:05:22Z
dc.date.available	2022-03-19T11:05:22Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=12090411
dc.identifier.citation	Geochimica et Cosmochimica Acta, 2004, 68, 22, 4649-4663
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36438
dc.description.abstract	Flow-through dissolution experiments were carried out on crushed granitoid rock (the Elat Granite) and three mineral separates (plagioclase, perthite, and biotite + chlorite) from this rock at pH 1 and 25°C. Major element concentrations were combined with Pb and Sr isotopic analyses of starting materials and output solutions and together enabled us to elucidate several important mechanisms related to granitoid rock weathering. We observed an initial stage of rock dissolution (
dc.title	LEAD AND STRONTIUM ISOTOPES AS MONITORS OF EXPERIMENTAL GRANITOID MINERAL DISSOLUTION
dc.type	Статья

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