Open Access Repository

Nickel-rich metasomatism of the lithospheric mantle by pre-kimberlitic alkali-S–Cl-rich C–O–H fluids


Downloads per month over past year

Giuliani, A, Kamenetsky, VS, Kendrick, MA, Phillips, D and Goemann, K 2013 , 'Nickel-rich metasomatism of the lithospheric mantle by pre-kimberlitic alkali-S–Cl-rich C–O–H fluids' , Contributions to Mineralology and Petrology, vol. 165, no. 1 , pp. 155-171 , doi: 10.1007/s00410-012-0801-1.

[img] PDF
CMP-Ni_metasoma...pdf | Request a copy
Full text restricted
Available under University of Tasmania Standard License.


Metasomatism of the lithospheric mantle sometimes produces unusual assemblages containing native metals and alloys, which provide important insight into metasomatic processes in the mantle. In this study, we describe the metasomatic enrichment of a refractory harzburgite xenolith in Ni, Fe and, to a lesser extent, Cu, Co, As and Sb. The xenolith (XM1/422) derives from the Bultfontein kimberlite (Kimberley, South Africa) and hosts Ni mineralisation that includes native nickel (Ni84.5-98.0), heazlewoodite (Ni3S2) and Ni-rich silicates (e.g. up to 37.5 wt % NiO in olivine, and 22.4 wt % NiO in phlogopite). The presence of several mineral phases enriched in alkali and volatile species (e.g. phlogopite, phosphates, carbonates, chlorides, djerfisherite) indicates that the transition metal cations were likely introduced during metasomatism by alkali-rich C–O–H fluids or alkali-carbonate melts. It is postulated that sulphide breakdown and fluid reaction with refractory mantle rocks contributed to the fluid’s enrichment in Ni and other metallic cations. The Ni-rich assemblages of xenolith XM1/422 show local chemical disequilibrium, and modelling of the Ni diffusion profiles adjacent to olivinenative nickel and olivine-heazlewoodite grain boundaries, suggests a close temporal relationship between Ni-rich metasomatism and subsequent entrainment by the kimberlite magma. However, metal-rich metasomatism has also been observed in other lithospheric mantle domains, including orogenic peridotitic massifs and the suboceanic mantle; regions unaffected by kimberlite magmatsim. As microscale occurrences of metallic phases are easily overlooked, it is possible that metal-rich metasomatism is more widespread in the Earth’s mantle than previously recognised.

Item Type: Article
Authors/Creators:Giuliani, A and Kamenetsky, VS and Kendrick, MA and Phillips, D and Goemann, K
Keywords: Native nickel � Olivine � Metasomatism �C–O–H fluids � Lithospheric mantle � Kimberlite
Journal or Publication Title: Contributions to Mineralology and Petrology
ISSN: 0010-7999 (Print), 1432-0967 (Online)
DOI / ID Number: 10.1007/s00410-012-0801-1
Item Statistics: View statistics for this item

Actions (login required)

Item Control Page Item Control Page