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dc.contributor.authorWasilewski, B.
dc.contributor.authorDoucet, Luc-Serge
dc.contributor.authorMoine, B.
dc.contributor.authorBeunon, H.
dc.contributor.authorDelpech, G.
dc.contributor.authorMattielli, N.
dc.contributor.authorDebaille, V.
dc.contributor.authorDelacour, A.
dc.contributor.authorGrï goire, M.
dc.contributor.authorGuillaume, D.
dc.contributor.authorCottin, J.
dc.date.accessioned2018-05-18T07:58:51Z
dc.date.available2018-05-18T07:58:51Z
dc.date.created2018-05-18T00:23:16Z
dc.date.issued2017
dc.identifier.citationWasilewski, B. and Doucet, L. and Moine, B. and Beunon, H. and Delpech, G. and Mattielli, N. and Debaille, V. et al. 2017. Ultra-refractory mantle within oceanic plateau: Petrology of the spinel harzburgites from Lac Michèle, Kerguelen Archipelago. Lithos. 272-273: pp. 336-349.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/67516
dc.identifier.doi10.1016/j.lithos.2016.12.010
dc.description.abstract

The study presents major and trace element compositions of whole-rocks and minerals of 24 spinel harzburgite xenoliths from the Lac Michèle locality in the northern part of the Kerguelen Archipelago (South Indian Ocean). The samples are modally homogeneous and large enough to provide representative whole-rock samples. Their Mg# are high (0.91 to 0.93) and they have 16–29 wt.% orthopyroxene (opx) and low clinopyroxene contents (0.1–2.8 wt.%). They display a wide range of serpentinisation, which result in LOI contents ranging from 0 to 3.5 wt.%. The spinel-bearing harzburgites from Lac Michèle are the most refractory peridotites identified so far among peridotite xenoliths available on the Kerguelen Archipelago and within the oceanic lithosphere. By contrast with most of the peridotite xenoliths from Kerguelen, they have been more preserved from post-formation processes such as metasomatic processes. The major and trace element compositions of the least serpentinised spinel harzburgites indicate an origin by ~ 30% of polybaric decompression fractional melting between 5GPa and ≤ 1 GPa. Thus, the spinel harzburgites from Lac Michèle, situated at the top of the Kerguelen lithospheric mantle, are residues of melting that took place over a broad range of depth and mostly in the garnet stability field. Our results, in comparison with published data on mantle xenoliths worldwide, show that spinel harzburgites from Lac Michèle have major and modal compositions that fall in the range of cratonic peridotites rather than abyssal peridotites, oceanic island peridotites, subduction zones peridotites and off-cratonic peridotites. This indicates (i) they formed in similar condition as for the ancient continental lithospheric mantle or (ii) they are fragment of ancient continental lithospheric mantle incorporated in the Kerguelen plateau.

dc.publisherElsevier BV
dc.titleUltra-refractory mantle within oceanic plateau: Petrology of the spinel harzburgites from Lac Michèle, Kerguelen Archipelago
dc.typeJournal Article
dcterms.source.volume272-273
dcterms.source.startPage336
dcterms.source.endPage349
dcterms.source.issn0024-4937
dcterms.source.titleLithos
curtin.departmentSchool of Earth and Planetary Sciences (EPS)
curtin.accessStatusFulltext not available


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