Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas

International audience We present the first combined Sm-146.147-Nd-142,Nd-143 and Lu-176-Hf-176 study of mafic rocks (amphibolites) from the western part of the Isua Supracrustal Belt (ISB, SW Greenland). Sm-Nd and Lu-Hf whole-rock isochrons yield identical ages within error: 3.72 +/- 0.08 and 3.67...

Full description

Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Rizo, Hanika, Boyet, Maud, Blichert-Toft, Janne, Rosing, Minik
Other Authors: Laboratoire Magmas et Volcans (LMV), Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Natural History Museum of Denmark, Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH), Nordic Centre of Earth Evolution (NORDCEE), University of Copenhagen = Københavns Universitet (UCPH), European Research Council under the European Community : 209035
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2011
Subjects:
Online Access:https://insu.hal.science/insu-00673487
https://doi.org/10.1016/j.epsl.2011.10.014
id ftunivlyon:oai:HAL:insu-00673487v1
record_format openpolar
institution Open Polar
collection Université de Lyon: HAL
op_collection_id ftunivlyon
language English
topic Hf isotopes
Nd isotopes
Nd-142
Isua amphibolites perovskite
Hadean
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle Hf isotopes
Nd isotopes
Nd-142
Isua amphibolites perovskite
Hadean
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
[SDE.MCG]Environmental Sciences/Global Changes
Rizo, Hanika
Boyet, Maud
Blichert-Toft, Janne
Rosing, Minik
Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas
topic_facet Hf isotopes
Nd isotopes
Nd-142
Isua amphibolites perovskite
Hadean
[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
[SDE.MCG]Environmental Sciences/Global Changes
description International audience We present the first combined Sm-146.147-Nd-142,Nd-143 and Lu-176-Hf-176 study of mafic rocks (amphibolites) from the western part of the Isua Supracrustal Belt (ISB, SW Greenland). Sm-Nd and Lu-Hf whole-rock isochrons yield identical ages within error: 3.72 +/- 0.08 and 3.67 +/- 0.07 Ga, respectively. Nd-142 measurements confirm and extend the database of Nd-142 excesses in Isua samples (mu Nd-142 = 7-16 ppm relative to the terrestrial Nd standard), indicating that early-differentiated reservoirs escaped complete homogenization by mantle convection until the Archean. Combined Sm-146,Sm-147-Nd-142,Nd-143 systematics suggest differentiation of the Isua amphibolite reservoir at maximum ages of similar to 4.53, similar to 4.47, and similar to 4.32 Ga. These ages are relative to, respectively, ordinary-chondritic, enstatite-chondritic, and higher-than-chondritic mantle compositions. The intercept of the Sm-Nd whole-rock isochron is in accordance with Nd-142 results and consistent with a superchondritic initial Nd-143/Nd-144 ratio (epsilon Nd-143(3.7Ga) = +1.41 +/- 0.98). In contrast, the corresponding initial epsilon Hf-176(3.7Ga) = -1.41 +/- 0.57 is subchondritic. Since Lu/Hf and Sm/Nd fractionate similarly during mantle processes, the Sm-Nd and Lu-Hf isotope systems display incongruent relative parent-daughter behavior in the source of Isua amphibolites. Based on high-pressure and -temperature phase partition coefficients, we propose a model that satisfies Sm-147-Nd-143, Lu-176-Hf-176, and Nd-142 results, as well as trace element characteristics. A deep-seated source composed largely of magnesium perovskite (98% MgPv) and containing 2% calcium perovskite satisfactorily explains the Nd and Hf isotopic discordance observed for Isua amphibolites. The negative HFSE anomalies characterizing Isua basalts likewise could have been inherited from such an early (4.53-4.32 Ga) deep mantle cumulate. Since the similar to 4 Ga old Acasta Gneisses (Northwest Territories, Canada) have radiogenic ...
author2 Laboratoire Magmas et Volcans (LMV)
Observatoire de Physique du Globe de Clermont-Ferrand (OPGC)
Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE)
École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL)
Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS)
Natural History Museum of Denmark
Faculty of Science Copenhagen
University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)
Nordic Centre of Earth Evolution (NORDCEE)
University of Copenhagen = Københavns Universitet (UCPH)
European Research Council under the European Community : 209035
format Article in Journal/Newspaper
author Rizo, Hanika
Boyet, Maud
Blichert-Toft, Janne
Rosing, Minik
author_facet Rizo, Hanika
Boyet, Maud
Blichert-Toft, Janne
Rosing, Minik
author_sort Rizo, Hanika
title Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas
title_short Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas
title_full Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas
title_fullStr Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas
title_full_unstemmed Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas
title_sort combined nd and hf isotope evidence for deep-seated source of isua lavas
publisher HAL CCSD
publishDate 2011
url https://insu.hal.science/insu-00673487
https://doi.org/10.1016/j.epsl.2011.10.014
genre Greenland
Northwest Territories
genre_facet Greenland
Northwest Territories
op_source ISSN: 0012-821X
Earth and Planetary Science Letters
https://insu.hal.science/insu-00673487
Earth and Planetary Science Letters, 2011, 312 (3-4), pp.267-279. ⟨10.1016/j.epsl.2011.10.014⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2011.10.014
insu-00673487
https://insu.hal.science/insu-00673487
doi:10.1016/j.epsl.2011.10.014
op_doi https://doi.org/10.1016/j.epsl.2011.10.014
container_title Earth and Planetary Science Letters
container_volume 312
container_issue 3-4
container_start_page 267
op_container_end_page 279
_version_ 1810447811699802112
spelling ftunivlyon:oai:HAL:insu-00673487v1 2024-09-15T18:10:12+00:00 Combined Nd and Hf isotope evidence for deep-seated source of Isua lavas Rizo, Hanika Boyet, Maud Blichert-Toft, Janne Rosing, Minik Laboratoire Magmas et Volcans (LMV) Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE) École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS) Natural History Museum of Denmark Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) Nordic Centre of Earth Evolution (NORDCEE) University of Copenhagen = Københavns Universitet (UCPH) European Research Council under the European Community : 209035 2011-12-15 https://insu.hal.science/insu-00673487 https://doi.org/10.1016/j.epsl.2011.10.014 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2011.10.014 insu-00673487 https://insu.hal.science/insu-00673487 doi:10.1016/j.epsl.2011.10.014 ISSN: 0012-821X Earth and Planetary Science Letters https://insu.hal.science/insu-00673487 Earth and Planetary Science Letters, 2011, 312 (3-4), pp.267-279. ⟨10.1016/j.epsl.2011.10.014⟩ Hf isotopes Nd isotopes Nd-142 Isua amphibolites perovskite Hadean [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2011 ftunivlyon https://doi.org/10.1016/j.epsl.2011.10.014 2024-07-08T23:59:50Z International audience We present the first combined Sm-146.147-Nd-142,Nd-143 and Lu-176-Hf-176 study of mafic rocks (amphibolites) from the western part of the Isua Supracrustal Belt (ISB, SW Greenland). Sm-Nd and Lu-Hf whole-rock isochrons yield identical ages within error: 3.72 +/- 0.08 and 3.67 +/- 0.07 Ga, respectively. Nd-142 measurements confirm and extend the database of Nd-142 excesses in Isua samples (mu Nd-142 = 7-16 ppm relative to the terrestrial Nd standard), indicating that early-differentiated reservoirs escaped complete homogenization by mantle convection until the Archean. Combined Sm-146,Sm-147-Nd-142,Nd-143 systematics suggest differentiation of the Isua amphibolite reservoir at maximum ages of similar to 4.53, similar to 4.47, and similar to 4.32 Ga. These ages are relative to, respectively, ordinary-chondritic, enstatite-chondritic, and higher-than-chondritic mantle compositions. The intercept of the Sm-Nd whole-rock isochron is in accordance with Nd-142 results and consistent with a superchondritic initial Nd-143/Nd-144 ratio (epsilon Nd-143(3.7Ga) = +1.41 +/- 0.98). In contrast, the corresponding initial epsilon Hf-176(3.7Ga) = -1.41 +/- 0.57 is subchondritic. Since Lu/Hf and Sm/Nd fractionate similarly during mantle processes, the Sm-Nd and Lu-Hf isotope systems display incongruent relative parent-daughter behavior in the source of Isua amphibolites. Based on high-pressure and -temperature phase partition coefficients, we propose a model that satisfies Sm-147-Nd-143, Lu-176-Hf-176, and Nd-142 results, as well as trace element characteristics. A deep-seated source composed largely of magnesium perovskite (98% MgPv) and containing 2% calcium perovskite satisfactorily explains the Nd and Hf isotopic discordance observed for Isua amphibolites. The negative HFSE anomalies characterizing Isua basalts likewise could have been inherited from such an early (4.53-4.32 Ga) deep mantle cumulate. Since the similar to 4 Ga old Acasta Gneisses (Northwest Territories, Canada) have radiogenic ... Article in Journal/Newspaper Greenland Northwest Territories Université de Lyon: HAL Earth and Planetary Science Letters 312 3-4 267 279