The Open UniversitySkip to content
 

Compositional controls on Ar-40/Ar-39 ages of zoned mica from a rare-element pegmatite

Smith, S.R; Kelley, S.P; Tindle, A.G and Breaks, F.W (2005). Compositional controls on Ar-40/Ar-39 ages of zoned mica from a rare-element pegmatite. Contributions to Mineralogy and Petrology, 149(5) pp. 613–626.

DOI (Digital Object Identifier) Link: http://dx.doi.org/10.1007/s00410-005-0674-7
Google Scholar: Look up in Google Scholar

Abstract

A high spatial resolution Ar-Ar dating study of compositionally zoned micas using UV laser extraction has been used to investigate the effect of composition and compositional boundaries upon argon diffusion in mica. The crystals are characterised by muscovite cores and Li-F-Rb-Cs-rich lepidolite rims produced by the interaction of a residual melt-vapour phase with the original muscovite during the late stages of pegmatite crystallisation. Single crystals exhibit dramatic intra-grain age variations, with a maximum range of 2,880-2,117 Ma. Backscattered electron images combined with UV-laser analyses reveal that apparent ages younger than 2,600 Ma are directly associated with the compositionally distinct rims, suggesting that Ar diffusion was faster in the lepidolite than in muscovite. Although it is not possible to be fully quantitative using the present data, it seems that argon diffusion rates in lepidolite are similar to those in biotite. Major rearrangements of the crystal structure needed to accommodate high concentrations of lithium, fluorine and large interlayer cations (Rb+, Cs+) in muscovite account for lower argon retentivity of the crystal rims. In most cases the age profiles show no disturbance at the compositional boundary, despite the transition from a di-octahedral to tri-octahedral mica, indicating that in general the boundaries do not act as fast diffusion pathways. However, in some cases there is a clear drop in ages at the compositional boundary, which acts as an effective sub-grain boundary. The difference between the two types may be related to the internal structure of the compositional boundaries or their degree of contact with the grain boundary network of the rock.

Item Type: Journal Article
ISSN: 0010-7999
Keywords: metamorphic calcic amphiboles; Northwestern Ontario; Superior Province; peraluminous granite; argon; retentivity; South Dakota; Black Hills; laser probe; muscovite; diffusion
Academic Unit/Department: Science > Environment, Earth and Ecosystems
Interdisciplinary Research Centre: Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)
Item ID: 2097
Depositing User: Simon Kelley
Date Deposited: 05 Jun 2006
Last Modified: 02 Dec 2010 19:46
URI: http://oro.open.ac.uk/id/eprint/2097
Share this page:

Actions (login may be required)

View Item
Report issue / request change

Policies | Disclaimer

© The Open University   + 44 (0)870 333 4340   general-enquiries@open.ac.uk