Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones

Co-auteur étranger International audience We report chlorine (Cl) and fluorine (F) abundances in minerals, interstitial glasses, and melt inclusions in 12 andesite-hosted, spinel harzburgite xenoliths and crosscutting pyroxenite veins exhumed from the sub-arc lithospheric mantle beneath Avacha volca...

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Published in:Geochimica et Cosmochimica Acta
Main Authors: Benard, A., Koga, K.T., Shimizu, N., Kendrick, M. A., Ionov, Dmitri, Nebel, O., Arculus, R. J.
Other Authors: Research School of Earth Sciences Canberra (RSES), Australian National University (ANU), Laboratoire Magmas et Volcans (LMV), Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS), Woods Hole Oceanographic Institution (WHOI), Géosciences Montpellier, Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Université des Antilles (UA), Monash University, Centre National de la Recherche Scientifique and Institut National des Sciences de l’Univers (PNP project, theme SEDI-TPS to D. A.), the Australian Research Council (DE120100513 to O. N. and DP120104240 to R. J. A and O. N.), ANR-10-LABX-0006,CLERVOLC,Clermont-Ferrand centre for research on volcanism(2010), ANR-16-IDEX-0001,CAP 20-25,CAP 20-25(2016)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-01553610
https://doi.org/10.1016/j.gca.2016.10.035
id ftunivnantes:oai:HAL:hal-01553610v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic peridotite
Partition coefficients
Island-arc
Subduction
Chlorine
Fluorine
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle peridotite
Partition coefficients
Island-arc
Subduction
Chlorine
Fluorine
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Benard, A.
Koga, K.T.
Shimizu, N.
Kendrick, M. A.
Ionov, Dmitri
Nebel, O.
Arculus, R. J.
Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones
topic_facet peridotite
Partition coefficients
Island-arc
Subduction
Chlorine
Fluorine
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description Co-auteur étranger International audience We report chlorine (Cl) and fluorine (F) abundances in minerals, interstitial glasses, and melt inclusions in 12 andesite-hosted, spinel harzburgite xenoliths and crosscutting pyroxenite veins exhumed from the sub-arc lithospheric mantle beneath Avacha volcano in the Kamchatka Arc (NE Russia). The data are used to calculate equilibrium mineral-melt partition coefficients (Dmineral/meltDmineral/melt) for Cl and F relevant to subduction-zone processes and unravel the history of volatile depletion and enrichment mechanisms in an arc setting.Chlorine is ∼100 times more incompatible in pyroxenes (View the MathML sourceDClmineral/melt = 0.005–0.008 [±0.002–0.003]) than F (View the MathML sourceDFmineral/melt = 0.50–0.57 [±0.21–0.24]), which indicates that partial melting of mantle sources leads to strong depletions in Cl relative to F in the residues. The data set in this study suggests a strong control of melt composition on View the MathML sourceDCl,Fpyroxene/melt, in particular H2O contents and Al/(Al + Si), which is in line with recent experiments. Fluorine is compatible in Ca-amphibole in the ‘wet’ sub-arc mantle (View the MathML sourceDFamphibole/melt = 3.5–3.7 [±1.5]) but not Cl (View the MathML sourceDClamphibole/melt = 0.03–0.05 [±0.01–0.03]), indicating that amphibole may fractionate F from Cl in the mantle wedge. The inter-mineral partition coefficients for Cl and F in this study are consistent amongst different harzburgite samples, whether they contain glass or not. In particular, disseminated amphibole hosts much of the Cl and F bulk rock budgets of spinel harzburgites (View the MathML sourceDClamphibole/pyroxene up to 14 and View the MathML sourceDFamphibole/pyroxene up to 40). Chlorine and fluorine are variably enriched (up to 1500 ppm Cl and 750 ppm F) in the parental arc picrite and boninite melts of primitive pyroxenite veins (and related melt inclusions) crosscutting spinel harzburgites.Based on the data in this study, the main inferences on the ...
author2 Research School of Earth Sciences Canberra (RSES)
Australian National University (ANU)
Laboratoire Magmas et Volcans (LMV)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)
Woods Hole Oceanographic Institution (WHOI)
Géosciences Montpellier
Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Université des Antilles (UA)
Monash University
Centre National de la Recherche Scientifique and Institut National des Sciences de l’Univers (PNP project, theme SEDI-TPS to D. A.)
the Australian Research Council (DE120100513 to O. N. and DP120104240 to R. J. A and O. N.)
ANR-10-LABX-0006,CLERVOLC,Clermont-Ferrand centre for research on volcanism(2010)
ANR-16-IDEX-0001,CAP 20-25,CAP 20-25(2016)
format Article in Journal/Newspaper
author Benard, A.
Koga, K.T.
Shimizu, N.
Kendrick, M. A.
Ionov, Dmitri
Nebel, O.
Arculus, R. J.
author_facet Benard, A.
Koga, K.T.
Shimizu, N.
Kendrick, M. A.
Ionov, Dmitri
Nebel, O.
Arculus, R. J.
author_sort Benard, A.
title Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones
title_short Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones
title_full Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones
title_fullStr Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones
title_full_unstemmed Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones
title_sort chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (kamchatka, russia): implications for melt generation and volatile recycling processes in subduction zones
publisher HAL CCSD
publishDate 2017
url https://hal.archives-ouvertes.fr/hal-01553610
https://doi.org/10.1016/j.gca.2016.10.035
long_lat ENVELOPE(158.503,158.503,53.040,53.040)
geographic Avacha
geographic_facet Avacha
genre Kamchatka
genre_facet Kamchatka
op_source ISSN: 0016-7037
EISSN: 0016-7037
Geochimica et Cosmochimica Acta
https://hal.archives-ouvertes.fr/hal-01553610
Geochimica et Cosmochimica Acta, Elsevier, 2017, 199, pp.324-350. ⟨10.1016/j.gca.2016.10.035⟩
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https://hal.archives-ouvertes.fr/hal-01553610
doi:10.1016/j.gca.2016.10.035
op_doi https://doi.org/10.1016/j.gca.2016.10.035
container_title Geochimica et Cosmochimica Acta
container_volume 199
container_start_page 324
op_container_end_page 350
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spelling ftunivnantes:oai:HAL:hal-01553610v1 2023-05-15T16:59:09+02:00 Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): Implications for melt generation and volatile recycling processes in subduction zones Benard, A. Koga, K.T. Shimizu, N. Kendrick, M. A. Ionov, Dmitri Nebel, O. Arculus, R. J. Research School of Earth Sciences Canberra (RSES) Australian National University (ANU) Laboratoire Magmas et Volcans (LMV) Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS) Woods Hole Oceanographic Institution (WHOI) Géosciences Montpellier Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Université des Antilles (UA) Monash University Centre National de la Recherche Scientifique and Institut National des Sciences de l’Univers (PNP project, theme SEDI-TPS to D. A.) the Australian Research Council (DE120100513 to O. N. and DP120104240 to R. J. A and O. N.) ANR-10-LABX-0006,CLERVOLC,Clermont-Ferrand centre for research on volcanism(2010) ANR-16-IDEX-0001,CAP 20-25,CAP 20-25(2016) 2017-02-15 https://hal.archives-ouvertes.fr/hal-01553610 https://doi.org/10.1016/j.gca.2016.10.035 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gca.2016.10.035 hal-01553610 https://hal.archives-ouvertes.fr/hal-01553610 doi:10.1016/j.gca.2016.10.035 ISSN: 0016-7037 EISSN: 0016-7037 Geochimica et Cosmochimica Acta https://hal.archives-ouvertes.fr/hal-01553610 Geochimica et Cosmochimica Acta, Elsevier, 2017, 199, pp.324-350. ⟨10.1016/j.gca.2016.10.035⟩ peridotite Partition coefficients Island-arc Subduction Chlorine Fluorine [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2017 ftunivnantes https://doi.org/10.1016/j.gca.2016.10.035 2022-08-10T06:56:11Z Co-auteur étranger International audience We report chlorine (Cl) and fluorine (F) abundances in minerals, interstitial glasses, and melt inclusions in 12 andesite-hosted, spinel harzburgite xenoliths and crosscutting pyroxenite veins exhumed from the sub-arc lithospheric mantle beneath Avacha volcano in the Kamchatka Arc (NE Russia). The data are used to calculate equilibrium mineral-melt partition coefficients (Dmineral/meltDmineral/melt) for Cl and F relevant to subduction-zone processes and unravel the history of volatile depletion and enrichment mechanisms in an arc setting.Chlorine is ∼100 times more incompatible in pyroxenes (View the MathML sourceDClmineral/melt = 0.005–0.008 [±0.002–0.003]) than F (View the MathML sourceDFmineral/melt = 0.50–0.57 [±0.21–0.24]), which indicates that partial melting of mantle sources leads to strong depletions in Cl relative to F in the residues. The data set in this study suggests a strong control of melt composition on View the MathML sourceDCl,Fpyroxene/melt, in particular H2O contents and Al/(Al + Si), which is in line with recent experiments. Fluorine is compatible in Ca-amphibole in the ‘wet’ sub-arc mantle (View the MathML sourceDFamphibole/melt = 3.5–3.7 [±1.5]) but not Cl (View the MathML sourceDClamphibole/melt = 0.03–0.05 [±0.01–0.03]), indicating that amphibole may fractionate F from Cl in the mantle wedge. The inter-mineral partition coefficients for Cl and F in this study are consistent amongst different harzburgite samples, whether they contain glass or not. In particular, disseminated amphibole hosts much of the Cl and F bulk rock budgets of spinel harzburgites (View the MathML sourceDClamphibole/pyroxene up to 14 and View the MathML sourceDFamphibole/pyroxene up to 40). Chlorine and fluorine are variably enriched (up to 1500 ppm Cl and 750 ppm F) in the parental arc picrite and boninite melts of primitive pyroxenite veins (and related melt inclusions) crosscutting spinel harzburgites.Based on the data in this study, the main inferences on the ... Article in Journal/Newspaper Kamchatka Université de Nantes: HAL-UNIV-NANTES Avacha ENVELOPE(158.503,158.503,53.040,53.040) Geochimica et Cosmochimica Acta 199 324 350