EMPIRICAL CALIBRATION OF OXYGEN ISOTOPE FRACTIONATION IN ZIRCON

dc.contributor.author	Valley J.W.
dc.contributor.author	Bindeman I.N.
dc.contributor.author	Peck W.H.
dc.date.accessioned	2021-12-02T03:58:07Z
dc.date.available	2021-12-02T03:58:07Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=14446085
dc.identifier.citation	Geochimica et Cosmochimica Acta, 2003, 67, 17, 3257-3266
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/32633
dc.description.abstract	New empirical calibrations for the fractionation of oxygen isotopes among zircon, almandine-rich garnet, titanite, and quartz are combined with experimental values for quartz-grossular. The resulting A-coefficients (‰K 2) are: for the relation 1000 ln Y-X A Y-X (10 6 /T 2). The fractionation of oxygen isotopes between zircon and coexisting minerals can provide otherwise unavailable evidence of magmatic processes, including crystalli-zation, remelting, and assimilation-fractional crystallization.
dc.subject	Zircon
dc.title	EMPIRICAL CALIBRATION OF OXYGEN ISOTOPE FRACTIONATION IN ZIRCON
dc.type	Статья

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