Rb/Sr isotopic and compositional retentivity of muscovite during deformation

Autor(en)

T. Eberlei, G. Habler, W. Wegner, R. Schuster, W. Koerner, M. Thoeni, R. Abart

Abstrakt

Permian metapegmatite muscovite from the Upper-Austroalpine Matsch Unit in Southern Tyrol (Italy) was investigated regarding its Rb/Sr and compositional retentivity during Cretaceous Upper-greenschist facies deformation. The data imply that microstructurally relic Permian magmatic muscovite largely maintained its major and trace element compositions during deformation, whereas the Rb/Sr geochronometer is strongly affected by a net loss of Sr. Lower Sr concentrations of muscovite correlate with higher ⁸⁷Rb/⁸⁶Sr and ⁸⁷Sr/⁸⁶Sr ratios. In most samples, the muscovite grain size- and magnetic-fractions with the lowest ⁸⁷Rb/⁸⁶Sr and ⁸⁷Sr/⁸⁶Sr ratios preserve a Permo-Triassic muscovite-whole rock Rb/Sr apparent age interpreted as to reflect formation during or cooling after pegmatite emplacement. Contrastingly, muscovite fractions with higher ⁸⁷Rb/⁸⁶Sr and ⁸⁷Sr/⁸⁶Sr ratios are arranged along a roughly linear array with a positive correlation of the ⁸⁷Rb/⁸⁶Sr and ⁸⁷Sr/⁸⁶Sr ratios in the ⁸⁷Rb/⁸⁶Sr vs ⁸⁷Sr/⁸⁶Sr space. They yield successively lower muscovite-whole rock Rb/Sr apparent ages. We explain the variations in the Rb/Sr isotopic character of microstructurally relic muscovite by a, presumably deformation-related, loss of Sr during the Cretaceous event. Contemporaneously, only very limited amounts of isotopically different Sr from the matrix reservoir might possibly have entered the muscovite. Consequently, the Rb/Sr of the relic muscovite is affected by a net loss of Sr. The results imply that at temperatures of <500°C, deformation is supposed to be the predominant factor in controlling the Rb/Sr geochronometer of relic muscovite, by significantly reducing the characteristic length scale for volume diffusion. However, variations of the major and trace element compositions within Permian relic muscovite are interpreted to rather reflect primary compositional instead of deformation-related variations.

Organisation(en)

Department für Lithosphärenforschung

Externe Organisation(en)

Geologische Bundesanstalt

Journal

Lithos

Band

227

Seiten

161-178

Anzahl der Seiten

18

ISSN

0024-4937

DOI

https://doi.org/10.1016/j.lithos.2015.04.007

Publikationsdatum

06-2015

Peer-reviewed

Ja

ÖFOS 2012

105120 Petrologie

Schlagwörter

ASJC Scopus Sachgebiete

Geochemistry and Petrology, Geology

Link zum Portal

https://ucrisportal.univie.ac.at/de/publications/rbsr-isotopic-and-compositional-retentivity-of-muscovite-during-deformation(fd4d33f2-1fe8-46af-bea2-00bea0779a99).html