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Chemistry of the Ta-Nb-Sn-W oxide minerals from the Yichun rare metal granite (SE China): genetic implications and comparison with Moroccan and French Hercynian examples

Published online by Cambridge University Press:  05 July 2018

M. Belkasmi
Affiliation:
Sidi Mohamed Ben Abdellah University, Department of Earth Sciences, BP. 1796, Fes-Atlas, Morocco
M. Cuney*
Affiliation:
CREGU-UMR G2R 7566, UHP, BP 239, F-54506, Vandú uvre Cedex, France
P. J. Pollard
Affiliation:
Economic Geology Research Unit, School of Earth Sciences, James Cook University, Townsville, Qld. 4811, Australia
A. Bastoul
Affiliation:
Ibn Tofail University, Department of Earth Sciences, BP 133, Kenitra, Morocco

Abstract

In the Yichun granite complex (SE China), columbite group minerals, microlite and cassiterite are the main Nb, Ta, Sn-bearing minerals. They are mainly concentrated in the uppermost albite-lepidolite granite. Rutile is the only Nb, Ta-bearing phase in the geochemically primitive muscovite-zinnwaldite granite. The chemical evolution of the columbite group minerals (the most abundant and commonly zoned Nb, Ta-bearing minerals) indicates a complex crystallization history of the host granites with: (1) fractional crystallization at depth, reflected by a strong increase of Mn/(Mn+Fe) ratios with a moderate increase of Ta/(Ta+Nb) ratios from the muscovite-zinnwaldite granite to the Li-mica granite and then the most fractionated topaz-lepidolite granite; and (2) emplacement of successive magma batches corresponding to the different units of the granite complex with progressive crystallization of each unit, mainly reflected by a strong increase of Ta/(Ta+Nb) ratios with moderate variation of Mn/(Mn+Fe) ratios during the growth of the zoned crystals. The data are compared with those from the RMG of Ezzirari (Morocco), Montebras, Beauvoir and Chèdeville (France).

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2000

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