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Excess <sup>40</sup>Ar in Alkali Feldspar and <sup>206,207</sup>Pb in Apatite Caused by Fluid-Induced Recrystallisation in a Semi-Closed Environment in Proterozoic (Meta)Granites of the Mt Isa Inlier, NE Australia

Interpretation of <sup>40</sup>Ar/<sup>39</sup>Ar dates of alkali feldspar and U-Pb dates of apatite depends on the dominant mechanism of isotopic transport in these minerals, which can be either diffusion or fluid-assisted dissolution-reprecipitation. To clarify the contributions of these processes...

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Detalles Bibliográficos
Principais autores: Daniil Popov, Richard Spikings, André Navin Paul, Maria Ovtcharova, Massimo Chiaradia, Martin Kutzschbach, Alexey Ulianov, Gary O’Sullivan, David Chew, Kalin Kouzmanov, Eszter Badenszki, J. Stephen Daly, Joshua H. F. L. Davies
Formato: Artigo
Idioma:Inglês
Publicado: MDPI AG 2024-12-01
Series:Geosciences
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Acceso en liña:https://www.mdpi.com/2076-3263/14/12/358
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