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Reaction aureoles around uraninites within biotite and plagioclase: evidence of low-temperature sequential fluid alteration and LREE-mobilization from monazite

Published online by Cambridge University Press:  02 January 2018

Manoj K. Ozha ,
Biswaji Mishra  and
Aiveliagaram V. Jeyagopal
Manoj K. Ozha
Affiliation:
Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India
Biswaji Mishra*
Affiliation:
Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India
Aiveliagaram V. Jeyagopal
Affiliation:
Atomic Minerals Directorate for Exploration and Research, Shillong 793019, India
*
*E-mail: [email protected]
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Abstract

Optical microscopy, Raman spectroscopy and electron probe microanalyses were conducted on a migmatitic metapelite to investigate the effects of alpha radiation and subsequent alteration at the interface between uraninite inclusions and the host minerals biotite, chlorite and albitic plagioclase. The study reveals (1) anomalous colouration under the polarizing microscope; (2) pertinent changes in the characteristic Raman spectra of host phases; (3) reaction aureoles, composed of secondary phases (viz. chlorite and K-feldspar) of various sizes (∼15–45 μm) within biotite and plagioclase, respectively; (iv) K-feldspatization and sericitization of plagioclase at the grain boundaries; (5) agreement between the observed α-penetration depths and the Monte-Carlo simulation results; and (6) dissolution textures within the matrix monazites. Analysis of the compositions of the reaction aureoles in albitic plagioclase reveals a systematic distribution of K-feldspar-, LREE- and clay-rich zones; while the same in biotite is composed of secondary chlorite. The growth sequence of the secondary phases indicates an influx of a K-rich fluid, following intense radiation damage, efficiently superimposed by LREE-metasomatism and later acidic alteration. These changes took place under low-temperature (≤150°C) conditions, wherein radial cracks (within plagioclase) and cleavages/fractures (within biotite) favoured fluid infiltration-circulation into the reaction aureoles. Depletion of the LREEs from the dissolved matrix monazites and their enrichment as a discrete LREE phase within the damaged aureoles in plagioclase demonstrate micrometre-scale LREE mobility.

Keywords

uraniniteradiation haloK-metasomatismLREE mobilization
Type
Research Article
Information
Mineralogical Magazine , Volume 80 , Issue 4 , June 2016 , pp. 567 - 584
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2016

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