Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism

Several spinel peridotite xenoliths from Spitsbergen have Sr-Nd isotopic compositions that plot to the right of the 'mantle array' defined by oceanic basalts and the DM end-member (depleted mantle, with low 87 Sr/86 Sr and high 143Nd/144 Nd). These xenoliths also show strong fractionation...

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Main Authors: Ionov, Dimitri, Mukasa, Samuel S.B., Bodinier, Jean-Louis
Format: Article in Journal/Newspaper
Language:English
Published: 2002
Subjects:
Online Access:http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/198714
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spelling ftunivbruxelles:oai:dipot.ulb.ac.be:2013/198714 2023-05-15T18:50:54+02:00 Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism Ionov, Dimitri Mukasa, Samuel S.B. Bodinier, Jean-Louis 2002-12 No full-text files http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/198714 en eng uri/info:scp/0036927638 http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/198714 Journal of Petrology, 43 (12 Géographie physique Pétrologie Géochimie Lithospheric mantle Metasomatism Radiogenic isotopes Spitsbergen Theoretical modelling info:eu-repo/semantics/article info:ulb-repo/semantics/articlePeerReview info:ulb-repo/semantics/openurl/article 2002 ftunivbruxelles 2022-06-12T20:34:28Z Several spinel peridotite xenoliths from Spitsbergen have Sr-Nd isotopic compositions that plot to the right of the 'mantle array' defined by oceanic basalts and the DM end-member (depleted mantle, with low 87 Sr/86 Sr and high 143Nd/144 Nd). These xenoliths also show strong fractionation of elements with similar compatibility (e.g. high La/Ce), which cannot be produced by simple mixing of light rare earth element-depleted peridotites with ocean island basalt-type or other enriched mantle melts. Numerical simulations of porous melt flow in spinel peridotites applied to Sr-Nd isotope compositions indicate that these features of the Spitsbergen peridotites can be explained by chemical fractionation during metasomatism in the mantle. 'Chromatographic' effects of melt percolation create a transient zone where the host depleted peridotites have experienced enrichment in Sr (with a radiogenic isotope composition) but not in Nd, thus producing Sr-Nd decoupling mainly controlled by partition coefficients and abundances of Sr and Nd in the melt and the peridotite. Therefore, Sr-Nd isotope decoupling, earlier reported for some other mantle peridotites worldwide, may be a signature of metasomatic processes rather than a source-related characteristic, contrary to models that invoke mixing with hypothetical Sr-rich fluids derived from subducted oceanic lithosphere. Pb isotope compositions of the Spitsbergen xenoliths do not appear to be consistently affected by the metasomatism. SCOPUS: ar.j info:eu-repo/semantics/published Article in Journal/Newspaper Ocean Island Spitsbergen DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB)
institution Open Polar
collection DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB)
op_collection_id ftunivbruxelles
language English
topic Géographie physique
Pétrologie
Géochimie
Lithospheric mantle
Metasomatism
Radiogenic isotopes
Spitsbergen
Theoretical modelling
spellingShingle Géographie physique
Pétrologie
Géochimie
Lithospheric mantle
Metasomatism
Radiogenic isotopes
Spitsbergen
Theoretical modelling
Ionov, Dimitri
Mukasa, Samuel S.B.
Bodinier, Jean-Louis
Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism
topic_facet Géographie physique
Pétrologie
Géochimie
Lithospheric mantle
Metasomatism
Radiogenic isotopes
Spitsbergen
Theoretical modelling
description Several spinel peridotite xenoliths from Spitsbergen have Sr-Nd isotopic compositions that plot to the right of the 'mantle array' defined by oceanic basalts and the DM end-member (depleted mantle, with low 87 Sr/86 Sr and high 143Nd/144 Nd). These xenoliths also show strong fractionation of elements with similar compatibility (e.g. high La/Ce), which cannot be produced by simple mixing of light rare earth element-depleted peridotites with ocean island basalt-type or other enriched mantle melts. Numerical simulations of porous melt flow in spinel peridotites applied to Sr-Nd isotope compositions indicate that these features of the Spitsbergen peridotites can be explained by chemical fractionation during metasomatism in the mantle. 'Chromatographic' effects of melt percolation create a transient zone where the host depleted peridotites have experienced enrichment in Sr (with a radiogenic isotope composition) but not in Nd, thus producing Sr-Nd decoupling mainly controlled by partition coefficients and abundances of Sr and Nd in the melt and the peridotite. Therefore, Sr-Nd isotope decoupling, earlier reported for some other mantle peridotites worldwide, may be a signature of metasomatic processes rather than a source-related characteristic, contrary to models that invoke mixing with hypothetical Sr-rich fluids derived from subducted oceanic lithosphere. Pb isotope compositions of the Spitsbergen xenoliths do not appear to be consistently affected by the metasomatism. SCOPUS: ar.j info:eu-repo/semantics/published
format Article in Journal/Newspaper
author Ionov, Dimitri
Mukasa, Samuel S.B.
Bodinier, Jean-Louis
author_facet Ionov, Dimitri
Mukasa, Samuel S.B.
Bodinier, Jean-Louis
author_sort Ionov, Dimitri
title Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism
title_short Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism
title_full Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism
title_fullStr Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism
title_full_unstemmed Sr-Nd-Pb isotopic compositions of peridotite xenoliths from Spitsbergen: Numerical modelling indicates Sr-Nd decoupling in the mantle by melt percolation metasomatism
title_sort sr-nd-pb isotopic compositions of peridotite xenoliths from spitsbergen: numerical modelling indicates sr-nd decoupling in the mantle by melt percolation metasomatism
publishDate 2002
url http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/198714
genre Ocean Island
Spitsbergen
genre_facet Ocean Island
Spitsbergen
op_source Journal of Petrology, 43 (12
op_relation uri/info:scp/0036927638
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/198714
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