Peridotite Weathering and Ni Redistribution in New Caledonian Laterite Profiles: Influence of Climate, Hydrology, and Structure

The peridotite massifs of New Caledonia are characterised by complex hydrodynamics influenced by intense inherited fracturing, uplift, and erosion. Following the formation of the erosion surfaces and alteration processes, these processes drive chemical redistribution during weathering; particularly...

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Veröffentlicht in:	Minerals (Basel) 2024-11, Vol.14 (11), p.1082
Hauptverfasser:	Cathelineau, Michel, Teitler, Yoram, Grimaud, Jean-Louis, Favier, Sylvain, Golfier, Fabrice, Ramanaidou, Erick, Grangeon, Sylvain, Kerreveur, Yohann, Jeanpert, Julie, Étienne, Samuel, Muñoz, Manuel, Ulrich, Marc
Format:	Artikel
Sprache:	eng
Schlagworte:	Boulders Cobalt Diffusion rate Dissolution Dissolving Earth Sciences Erosion surfaces Fractures Fronts Geomorphology Goethite Hydrodynamics Hydrology Iron oxides Laterites Magnesium Mass transfer Massifs Minerals Nickel Nontronite Oligocene Olivine Peridotite Permeability Renewal Sciences of the Universe Silica Topography Trace elements Weathering
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