NANOSCALE OCCURRENCE OF PB IN AN ARCHEAN ZIRCON

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dc.contributor.author Utsunomiya S.
dc.contributor.author Palenik C.S.
dc.contributor.author Ewing R.C.
dc.contributor.author Valley J.W.
dc.contributor.author Cavosie A.J.
dc.contributor.author Wilde S.A.
dc.date.accessioned 2022-07-11T05:35:39Z
dc.date.available 2022-07-11T05:35:39Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=31605877
dc.identifier.citation Geochimica et Cosmochimica Acta, 2004, 68, 22, 4679-4686
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38116
dc.description.abstract We report, for the first time, a direct, atomic-scale characterization of Pb in zircon (4.4 3.1 Ga) from the early Archean Yilgarn craton in Australia using high-resolution HAADF-STEM. Two forms of Pb have been identified: Pb concentrated at ˜3 atom% as a nanoscale patch in zircon structure, and Pb concentrated within the amorphous domain created by fission fragment damage. The first result suggests that the Pb atoms directly substitute for Zr4+ in the zircon structure, and the latter observation demonstrates that Pb diffusion can occur through amorphous regions created by radiation damage, although volume diffusion is typically considered to be the dominant mechanism for Pb diffusion. Beyond the first percolation point, i.e., when the amorphous domains overlap and form a fully interconnected network of amorphous domains, there is a new pathway for the diffusion of Pb that is faster than volume diffusion through crystalline zircon.
dc.subject Archean
dc.title NANOSCALE OCCURRENCE OF PB IN AN ARCHEAN ZIRCON
dc.type Статья
dc.subject.age Precambrian::Archean
dc.subject.age Докембрий::Архей ru


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