STRONTIUM DIFFUSION IN SANIDINE AND ALBITE, AND GENERAL COMMENTS ON STRONTIUM DIFFUSION IN ALKALI FELDSPARS

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dc.contributor.author Cherniak D.J.
dc.date.accessioned 2020-11-23T10:55:16Z
dc.date.available 2020-11-23T10:55:16Z
dc.date.issued 1996
dc.identifier https://elibrary.ru/item.asp?id=491657
dc.identifier.citation Geochimica et Cosmochimica Acta, 1996, , 24, 5037-5043
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/19420
dc.description.abstract Strontium chemical diffusion has been measured in albite and sanidine under dry, 1 atm, and QFM buffered conditions. Strontium oxide-aluminosilicate powdered sources were used to introduce the diffusant and Rutherford Backscattering Spectroscopy (RBS) used to measure diffusion profiles. For the 1 atm experiments, the following Arrhenius relations were obtained: Sanidine (Or61), temperature range 725-1075°C, diffusion normal to (001):D = 8.4 exp(-450 +/- 13 kJ mol-1/RT) m2s-1. Albite (Or1), temperature range 675-1025°C, diffusion normal to (001):D = 2.9 x 10-9 exp(-224 +/- 11 kJ mol-1/RT) m2s-1. The alkali feldspars in this and earlier work display a broad range of activation energies for Sr diffusion, which may be a consequence of the thermodynamic non-ideality of the alkali feldspar system and/or the mixed alkali effect.
dc.title STRONTIUM DIFFUSION IN SANIDINE AND ALBITE, AND GENERAL COMMENTS ON STRONTIUM DIFFUSION IN ALKALI FELDSPARS
dc.type Статья


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