Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques
International audience Samples collected during the PACANTARCTIC 2 cruise fill a sampling gap from 53° to 41° S along the Pacific Antarctic Ridge (PAR). Analysis of Sr, Nd, Pb, Hf, and He isotope compositions of these new samples is shown together with published data from 66°S to 53°S and from the E...
Published in: | Earth and Planetary Science Letters |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2011
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Subjects: | |
Online Access: | https://hal-insu.archives-ouvertes.fr/insu-00588804 https://hal-insu.archives-ouvertes.fr/insu-00588804/document https://hal-insu.archives-ouvertes.fr/insu-00588804/file/EPSL-Hamelin_al-2011.pdf https://doi.org/10.1016/j.epsl.2010.12.007 |
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Université de Bretagne Occidentale: HAL |
op_collection_id |
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language |
English |
topic |
oceanic basalts Pacific-Antarctic Ridge mantle heterogeneity Principal Component Analysis Sr Nd Pb Hf isotopes [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
oceanic basalts Pacific-Antarctic Ridge mantle heterogeneity Principal Component Analysis Sr Nd Pb Hf isotopes [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes Hamelin, Cédric Dosso, Laure Hanan, Barry B. Moreira, Manuel Kositsky, Andrew Thomas, Marion Y. Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques |
topic_facet |
oceanic basalts Pacific-Antarctic Ridge mantle heterogeneity Principal Component Analysis Sr Nd Pb Hf isotopes [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience Samples collected during the PACANTARCTIC 2 cruise fill a sampling gap from 53° to 41° S along the Pacific Antarctic Ridge (PAR). Analysis of Sr, Nd, Pb, Hf, and He isotope compositions of these new samples is shown together with published data from 66°S to 53°S and from the EPR. The recent advance in analytical mass spectrometry techniques generates a spectacular increase in the number of multidimensional isotopic data for oceanic basalts. Working with such multidimensional datasets generates a new approach for the data interpretation, preferably based on statistical analysis techniques. Principal Component Analysis (PCA) is a powerful mathematical tool to study this type of datasets. The purpose of PCA is to reduce the number of dimensions by keeping only those characteristics that contribute most to its variance. Using this technique, it becomes possible to have a statistical picture of the geochemical variations along the entire Pacific Ridge from 70°S to 10°S. The incomplete sampling of the ridge led previously to the identification of a large-scale division of the south Pacific mantle at the latitude of Easter Island. The PCA method applied here to the completed dataset reveals a different geochemical profile. Along the Pacific Ridge, a large-scale bell-shaped variation with an extremum at about 38°S of latitude is interpreted as a progressive change in the geochemical characteristics of the depleted matrix of the mantle. This Pacific Isotopic Bump (PIB) is also noticeable in the He isotopic ratio along-axis variation. The linear correlation observed between He and heavy radiogenic isotopes, together with the result of the PCA calculation, suggests that the large-scale variation is unrelated to the plume-ridge interactions in the area and should rather be attributed to the partial melting of a marble-cake assemblage. Research Highlights ► New Sr, Nd, Pb, Hf, and He isotopes data fill a sampling gap along the Pacific Ridge. ► We examine geochemical variation in MORB using a ... |
author2 |
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) Department of Geological Sciences San Diego State Univ (Geology SDSU) San Diego State University (SDSU) Institut de Physique du Globe de Paris (IPGP) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS) Tectonics Observatory California Institute of Technology (CALTECH) |
format |
Article in Journal/Newspaper |
author |
Hamelin, Cédric Dosso, Laure Hanan, Barry B. Moreira, Manuel Kositsky, Andrew Thomas, Marion Y. |
author_facet |
Hamelin, Cédric Dosso, Laure Hanan, Barry B. Moreira, Manuel Kositsky, Andrew Thomas, Marion Y. |
author_sort |
Hamelin, Cédric |
title |
Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques |
title_short |
Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques |
title_full |
Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques |
title_fullStr |
Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques |
title_full_unstemmed |
Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques |
title_sort |
geochemical portray of the pacific ridge: new isotopic data and statistical techniques |
publisher |
HAL CCSD |
publishDate |
2011 |
url |
https://hal-insu.archives-ouvertes.fr/insu-00588804 https://hal-insu.archives-ouvertes.fr/insu-00588804/document https://hal-insu.archives-ouvertes.fr/insu-00588804/file/EPSL-Hamelin_al-2011.pdf https://doi.org/10.1016/j.epsl.2010.12.007 |
geographic |
Antarctic Pacific |
geographic_facet |
Antarctic Pacific |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
ISSN: 0012-821X Earth and Planetary Science Letters https://hal-insu.archives-ouvertes.fr/insu-00588804 Earth and Planetary Science Letters, 2011, 302 (1-2), pp.154-162. ⟨10.1016/j.epsl.2010.12.007⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2010.12.007 insu-00588804 https://hal-insu.archives-ouvertes.fr/insu-00588804 https://hal-insu.archives-ouvertes.fr/insu-00588804/document https://hal-insu.archives-ouvertes.fr/insu-00588804/file/EPSL-Hamelin_al-2011.pdf doi:10.1016/j.epsl.2010.12.007 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.epsl.2010.12.007 |
container_title |
Earth and Planetary Science Letters |
container_volume |
302 |
container_issue |
1-2 |
container_start_page |
154 |
op_container_end_page |
162 |
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1768378919253180416 |
spelling |
ftunivbrest:oai:HAL:insu-00588804v1 2023-06-11T04:06:47+02:00 Geochemical portray of the Pacific Ridge: New isotopic data and statistical techniques Hamelin, Cédric Dosso, Laure Hanan, Barry B. Moreira, Manuel Kositsky, Andrew Thomas, Marion Y. 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) Department of Geological Sciences San Diego State Univ (Geology SDSU) San Diego State University (SDSU) Institut de Physique du Globe de Paris (IPGP) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS) Tectonics Observatory California Institute of Technology (CALTECH) 2011-02-01 https://hal-insu.archives-ouvertes.fr/insu-00588804 https://hal-insu.archives-ouvertes.fr/insu-00588804/document https://hal-insu.archives-ouvertes.fr/insu-00588804/file/EPSL-Hamelin_al-2011.pdf https://doi.org/10.1016/j.epsl.2010.12.007 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2010.12.007 insu-00588804 https://hal-insu.archives-ouvertes.fr/insu-00588804 https://hal-insu.archives-ouvertes.fr/insu-00588804/document https://hal-insu.archives-ouvertes.fr/insu-00588804/file/EPSL-Hamelin_al-2011.pdf doi:10.1016/j.epsl.2010.12.007 info:eu-repo/semantics/OpenAccess ISSN: 0012-821X Earth and Planetary Science Letters https://hal-insu.archives-ouvertes.fr/insu-00588804 Earth and Planetary Science Letters, 2011, 302 (1-2), pp.154-162. ⟨10.1016/j.epsl.2010.12.007⟩ oceanic basalts Pacific-Antarctic Ridge mantle heterogeneity Principal Component Analysis Sr Nd Pb Hf isotopes [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2011 ftunivbrest https://doi.org/10.1016/j.epsl.2010.12.007 2023-05-02T22:36:18Z International audience Samples collected during the PACANTARCTIC 2 cruise fill a sampling gap from 53° to 41° S along the Pacific Antarctic Ridge (PAR). Analysis of Sr, Nd, Pb, Hf, and He isotope compositions of these new samples is shown together with published data from 66°S to 53°S and from the EPR. The recent advance in analytical mass spectrometry techniques generates a spectacular increase in the number of multidimensional isotopic data for oceanic basalts. Working with such multidimensional datasets generates a new approach for the data interpretation, preferably based on statistical analysis techniques. Principal Component Analysis (PCA) is a powerful mathematical tool to study this type of datasets. The purpose of PCA is to reduce the number of dimensions by keeping only those characteristics that contribute most to its variance. Using this technique, it becomes possible to have a statistical picture of the geochemical variations along the entire Pacific Ridge from 70°S to 10°S. The incomplete sampling of the ridge led previously to the identification of a large-scale division of the south Pacific mantle at the latitude of Easter Island. The PCA method applied here to the completed dataset reveals a different geochemical profile. Along the Pacific Ridge, a large-scale bell-shaped variation with an extremum at about 38°S of latitude is interpreted as a progressive change in the geochemical characteristics of the depleted matrix of the mantle. This Pacific Isotopic Bump (PIB) is also noticeable in the He isotopic ratio along-axis variation. The linear correlation observed between He and heavy radiogenic isotopes, together with the result of the PCA calculation, suggests that the large-scale variation is unrelated to the plume-ridge interactions in the area and should rather be attributed to the partial melting of a marble-cake assemblage. Research Highlights ► New Sr, Nd, Pb, Hf, and He isotopes data fill a sampling gap along the Pacific Ridge. ► We examine geochemical variation in MORB using a ... Article in Journal/Newspaper Antarc* Antarctic Université de Bretagne Occidentale: HAL Antarctic Pacific Earth and Planetary Science Letters 302 1-2 154 162 |