Platinum and palladium mobility in supergene environment: The residual origin of the Pirogues River mineralization, New Caledonia

Eluvial concentration of platinum-group minerals (PGM) has developed in the south of New Caledonia, from the weathering of a mafic and ultramafic cumulate. The platinum/palladium (Pt/Pd) ratio evolution from the bottom to the top of the weathering profile indicates a chemical mobilization of Pd in s...

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Veröffentlicht in:Journal of geochemical exploration 2006-01, Vol.88 (1), p.350-354
Hauptverfasser: Traoré, D., Beauvais, A., Augé, T., Chabaux, F., Parisot, J.-C., Cathelineau, M., Peiffert, C., Colin, F.
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container_end_page 354
container_issue 1
container_start_page 350
container_title Journal of geochemical exploration
container_volume 88
creator Traoré, D.
Beauvais, A.
Augé, T.
Chabaux, F.
Parisot, J.-C.
Cathelineau, M.
Peiffert, C.
Colin, F.
description Eluvial concentration of platinum-group minerals (PGM) has developed in the south of New Caledonia, from the weathering of a mafic and ultramafic cumulate. The platinum/palladium (Pt/Pd) ratio evolution from the bottom to the top of the weathering profile indicates a chemical mobilization of Pd in supergene environment. The examination by scanning electron microscopy of the residual PGM collected in the weathering profile and their chemical characterization by electronic microprobe show a preservation of the structure and chemical signature (in the core of the grains) of the fresh PGM. This clearly demonstrates that the PGM studied here are residual and are affected by dissolution process.
doi_str_mv 10.1016/j.gexplo.2005.08.073
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subjects Earth Sciences
New Caledonia
Palladium
Platinum
Sciences of the Universe
Weathering
title Platinum and palladium mobility in supergene environment: The residual origin of the Pirogues River mineralization, New Caledonia
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