Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines)
International audience The Monglo adakite contains mafic and ultramafic xenoliths, which probably originated from the mantle section of an Early Cretaceous supra-subduction zone ophiolitic complex located within the Luzon arc crust. Spinel-bearing dunites are dominant among this xenolith collection...
Published in: | Lithos |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2008
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Subjects: | |
Online Access: | https://insu.hal.science/insu-00256478 https://insu.hal.science/insu-00256478/document https://insu.hal.science/insu-00256478/file/Gregoire-Lithos-2008.pdf https://doi.org/10.1016/j.lithos.2007.10.013 |
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institution |
Open Polar |
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Météo-France: HAL |
op_collection_id |
ftmeteofrance |
language |
English |
topic |
mantle xenoliths Luzon arc metasomatism dunite trace elements adakite 91.40.Rs [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
mantle xenoliths Luzon arc metasomatism dunite trace elements adakite 91.40.Rs [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes Grégoire, M. Jégo, Sébastien Maury, René Payot, Betchaida D. Tamayo, Rodolfo A. Yumul, Graciano P. Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines) |
topic_facet |
mantle xenoliths Luzon arc metasomatism dunite trace elements adakite 91.40.Rs [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience The Monglo adakite contains mafic and ultramafic xenoliths, which probably originated from the mantle section of an Early Cretaceous supra-subduction zone ophiolitic complex located within the Luzon arc crust. Spinel-bearing dunites are dominant among this xenolith collection and display evidence for three episodes of subduction-related melt percolation. The first one is evidenced by an undeformed clinopyroxene characterized by convex-upwards REE pattern. This clinopyroxene crystallized from a calc-alkaline basaltic magma, likely formed in the Cretaceous supra-subduction setting of the ophiolite. Then, two metasomatic events, evidenced by orthopyroxene-rich and amphibole-rich secondary parageneses, respectively, affected most of the spinel dunites. The opx-rich paragenesis is related to the circulation within the dunitic upper mantle of hydrous slab-derived melts similar to those affecting the mantle peridotite xenoliths from Papua New Guinea and Kamchatka. Finally the amphibole-rich veins are related to the interaction between the studied dunite xenoliths and the host adakite or an adakitic melt similar to it. |
author2 |
Dynamique terrestre et planétaire (DTP) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Institut des Sciences de la Terre d'Orléans (ISTO) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Philippine Council for Industry and Energy Research and Development-DOST National Institute of Geological Sciences Philippines Univ (NIGS UP) University of the Philippines Diliman (UP Diliman) Fieldwork and laboratory studies have been conducted with the financial and logistic help of UP-Diliman, the DUO-France program, the Ministère des Affaires Etrangères (French Embassy in Manila), the SUCRI program “Asie du Sud-Est”, Université de Bretagne Occidentale, Brest and of the CNRS and Université Toulouse III. |
format |
Article in Journal/Newspaper |
author |
Grégoire, M. Jégo, Sébastien Maury, René Payot, Betchaida D. Tamayo, Rodolfo A. Yumul, Graciano P. |
author_facet |
Grégoire, M. Jégo, Sébastien Maury, René Payot, Betchaida D. Tamayo, Rodolfo A. Yumul, Graciano P. |
author_sort |
Grégoire, M. |
title |
Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines) |
title_short |
Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines) |
title_full |
Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines) |
title_fullStr |
Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines) |
title_full_unstemmed |
Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines) |
title_sort |
metasomatic interactions between slab-derived melts and depleted mantle: insights from xenoliths within monglo adakite (luzon arc, philippines) |
publisher |
HAL CCSD |
publishDate |
2008 |
url |
https://insu.hal.science/insu-00256478 https://insu.hal.science/insu-00256478/document https://insu.hal.science/insu-00256478/file/Gregoire-Lithos-2008.pdf https://doi.org/10.1016/j.lithos.2007.10.013 |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
ISSN: 0024-4937 Lithos https://insu.hal.science/insu-00256478 Lithos, 2008, 103 (3-4), pp.415-430. ⟨10.1016/j.lithos.2007.10.013⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.lithos.2007.10.013 insu-00256478 https://insu.hal.science/insu-00256478 https://insu.hal.science/insu-00256478/document https://insu.hal.science/insu-00256478/file/Gregoire-Lithos-2008.pdf doi:10.1016/j.lithos.2007.10.013 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.lithos.2007.10.013 |
container_title |
Lithos |
container_volume |
103 |
container_issue |
3-4 |
container_start_page |
415 |
op_container_end_page |
430 |
_version_ |
1810453970237259776 |
spelling |
ftmeteofrance:oai:HAL:insu-00256478v1 2024-09-15T18:16:00+00:00 Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines) Grégoire, M. Jégo, Sébastien Maury, René Payot, Betchaida D. Tamayo, Rodolfo A. Yumul, Graciano P. Dynamique terrestre et planétaire (DTP) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Institut des Sciences de la Terre d'Orléans (ISTO) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Philippine Council for Industry and Energy Research and Development-DOST National Institute of Geological Sciences Philippines Univ (NIGS UP) University of the Philippines Diliman (UP Diliman) Fieldwork and laboratory studies have been conducted with the financial and logistic help of UP-Diliman, the DUO-France program, the Ministère des Affaires Etrangères (French Embassy in Manila), the SUCRI program “Asie du Sud-Est”, Université de Bretagne Occidentale, Brest and of the CNRS and Université Toulouse III. 2008 https://insu.hal.science/insu-00256478 https://insu.hal.science/insu-00256478/document https://insu.hal.science/insu-00256478/file/Gregoire-Lithos-2008.pdf https://doi.org/10.1016/j.lithos.2007.10.013 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.lithos.2007.10.013 insu-00256478 https://insu.hal.science/insu-00256478 https://insu.hal.science/insu-00256478/document https://insu.hal.science/insu-00256478/file/Gregoire-Lithos-2008.pdf doi:10.1016/j.lithos.2007.10.013 info:eu-repo/semantics/OpenAccess ISSN: 0024-4937 Lithos https://insu.hal.science/insu-00256478 Lithos, 2008, 103 (3-4), pp.415-430. ⟨10.1016/j.lithos.2007.10.013⟩ mantle xenoliths Luzon arc metasomatism dunite trace elements adakite 91.40.Rs [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2008 ftmeteofrance https://doi.org/10.1016/j.lithos.2007.10.013 2024-06-25T00:16:12Z International audience The Monglo adakite contains mafic and ultramafic xenoliths, which probably originated from the mantle section of an Early Cretaceous supra-subduction zone ophiolitic complex located within the Luzon arc crust. Spinel-bearing dunites are dominant among this xenolith collection and display evidence for three episodes of subduction-related melt percolation. The first one is evidenced by an undeformed clinopyroxene characterized by convex-upwards REE pattern. This clinopyroxene crystallized from a calc-alkaline basaltic magma, likely formed in the Cretaceous supra-subduction setting of the ophiolite. Then, two metasomatic events, evidenced by orthopyroxene-rich and amphibole-rich secondary parageneses, respectively, affected most of the spinel dunites. The opx-rich paragenesis is related to the circulation within the dunitic upper mantle of hydrous slab-derived melts similar to those affecting the mantle peridotite xenoliths from Papua New Guinea and Kamchatka. Finally the amphibole-rich veins are related to the interaction between the studied dunite xenoliths and the host adakite or an adakitic melt similar to it. Article in Journal/Newspaper Kamchatka Météo-France: HAL Lithos 103 3-4 415 430 |