Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton
Despite the scientific and economic significance of kimberlites and related magmas, their origin is unclear. Here, we address this issue using whole-rock and perovskite-derived Sr-Nd-Hf isotopes for the three occurrences of kimberlite, lamproites and ultramafic lamprophyres (UMLs) in Finland. Mesopr...
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ftethz:oai:www.research-collection.ethz.ch:20.500.11850/565143 2023-05-15T17:00:13+02:00 Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton Dalton, Hayden Giuliani, Andrea Hergt, Janet Phillips, David O'Brien, Hugh Ballmer, Maxim D. Maas, Roland Woodhead, Jon 2022-08 application/application/pdf https://hdl.handle.net/20.500.11850/565143 https://doi.org/10.3929/ethz-b-000565143 en eng Wiley info:eu-repo/semantics/altIdentifier/doi/10.1029/2021GC010324 info:eu-repo/semantics/altIdentifier/wos/000838102300001 info:eu-repo/grantAgreement/SNF/Ambizione/180126 http://hdl.handle.net/20.500.11850/565143 doi:10.3929/ethz-b-000565143 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International CC-BY Geochemistry, Geophysics, Geosystems, 23 (8) kimberlite geochemistry radiogenic isotopes geodynamics LLSVP mantle plumes info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftethz https://doi.org/20.500.11850/565143 https://doi.org/10.3929/ethz-b-000565143 https://doi.org/10.1029/2021GC010324 2023-02-13T01:09:31Z Despite the scientific and economic significance of kimberlites and related magmas, their origin is unclear. Here, we address this issue using whole-rock and perovskite-derived Sr-Nd-Hf isotopes for the three occurrences of kimberlite, lamproites and ultramafic lamprophyres (UMLs) in Finland. Mesoproterozoic olivine lamproites at Lentiira-Kuhmo and UMLs at Kuusamo have different isotopic signatures yet were emplaced contemporaneously at 1,200 Ma in response to an extensional regime linked to the Baltica-Laurentia breakup. The low epsilon Nd-(i) and epsilon Hf-(i) values of the olivine lamproites are consistent with an enriched subcontinental lithospheric mantle (SCLM) source while UML compositions are intermediate between those of typical kimberlites and lamproites and are interpreted to reflect mixing of asthenospheric melts and similar to 10%-15% of melts sourced from metasomatized SCLM. The similar to 750 Ma Kuusamo kimberlites, are probably linked to the mantle plume activity that initiated Rodinia's break-up, exhibiting homogenous isotopic compositions which mirror the prominent Geodynamic and Source Constraints for similar to 1,200 Ma Olivine Lamproite and Ultramafic Lamprophyre Magmatism in Eastern Finland (PREMA)-like signature of kimberlites globally. By contrast, similar to 620-585 Ma Kaavi-Kuopio kimberlites show limited range in epsilon Nd-(i) and Sr-87/Sr-86((i)) but have remarkably heterogeneous epsilon Hf-(i) (+6.5 to -6.3) with a temporal trend toward lower epsilon Hf-(i) values. While the Kuusamo kimberlites erupted during the early stage of continental break-up, the Kaavi-Kuopio kimberlites were emplaced when Rodinia break-up was completed, coeval with formation of the Central Iapetus large igneous province. Magmas forming the Kaavi-Kupio kimberlites may have formed from an upwelling mantle source similar to PREMA modified by increasing incorporation (up to 10%) of recycled crustal material through time accounting for the trend toward lower epsilon Hf-(i) in these kimberlites. ISSN:1525-2027 Article in Journal/Newspaper karelia* karelian ETH Zürich Research Collection Kuusamo ENVELOPE(29.183,29.183,65.967,65.967) |
institution |
Open Polar |
collection |
ETH Zürich Research Collection |
op_collection_id |
ftethz |
language |
English |
topic |
kimberlite geochemistry radiogenic isotopes geodynamics LLSVP mantle plumes |
spellingShingle |
kimberlite geochemistry radiogenic isotopes geodynamics LLSVP mantle plumes Dalton, Hayden Giuliani, Andrea Hergt, Janet Phillips, David O'Brien, Hugh Ballmer, Maxim D. Maas, Roland Woodhead, Jon Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton |
topic_facet |
kimberlite geochemistry radiogenic isotopes geodynamics LLSVP mantle plumes |
description |
Despite the scientific and economic significance of kimberlites and related magmas, their origin is unclear. Here, we address this issue using whole-rock and perovskite-derived Sr-Nd-Hf isotopes for the three occurrences of kimberlite, lamproites and ultramafic lamprophyres (UMLs) in Finland. Mesoproterozoic olivine lamproites at Lentiira-Kuhmo and UMLs at Kuusamo have different isotopic signatures yet were emplaced contemporaneously at 1,200 Ma in response to an extensional regime linked to the Baltica-Laurentia breakup. The low epsilon Nd-(i) and epsilon Hf-(i) values of the olivine lamproites are consistent with an enriched subcontinental lithospheric mantle (SCLM) source while UML compositions are intermediate between those of typical kimberlites and lamproites and are interpreted to reflect mixing of asthenospheric melts and similar to 10%-15% of melts sourced from metasomatized SCLM. The similar to 750 Ma Kuusamo kimberlites, are probably linked to the mantle plume activity that initiated Rodinia's break-up, exhibiting homogenous isotopic compositions which mirror the prominent Geodynamic and Source Constraints for similar to 1,200 Ma Olivine Lamproite and Ultramafic Lamprophyre Magmatism in Eastern Finland (PREMA)-like signature of kimberlites globally. By contrast, similar to 620-585 Ma Kaavi-Kuopio kimberlites show limited range in epsilon Nd-(i) and Sr-87/Sr-86((i)) but have remarkably heterogeneous epsilon Hf-(i) (+6.5 to -6.3) with a temporal trend toward lower epsilon Hf-(i) values. While the Kuusamo kimberlites erupted during the early stage of continental break-up, the Kaavi-Kuopio kimberlites were emplaced when Rodinia break-up was completed, coeval with formation of the Central Iapetus large igneous province. Magmas forming the Kaavi-Kupio kimberlites may have formed from an upwelling mantle source similar to PREMA modified by increasing incorporation (up to 10%) of recycled crustal material through time accounting for the trend toward lower epsilon Hf-(i) in these kimberlites. ISSN:1525-2027 |
format |
Article in Journal/Newspaper |
author |
Dalton, Hayden Giuliani, Andrea Hergt, Janet Phillips, David O'Brien, Hugh Ballmer, Maxim D. Maas, Roland Woodhead, Jon |
author_facet |
Dalton, Hayden Giuliani, Andrea Hergt, Janet Phillips, David O'Brien, Hugh Ballmer, Maxim D. Maas, Roland Woodhead, Jon |
author_sort |
Dalton, Hayden |
title |
Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton |
title_short |
Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton |
title_full |
Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton |
title_fullStr |
Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton |
title_full_unstemmed |
Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton |
title_sort |
geodynamic and isotopic constraints on the genesis of kimberlites, lamproites and related magmas from the finnish segment of the karelian craton |
publisher |
Wiley |
publishDate |
2022 |
url |
https://hdl.handle.net/20.500.11850/565143 https://doi.org/10.3929/ethz-b-000565143 |
long_lat |
ENVELOPE(29.183,29.183,65.967,65.967) |
geographic |
Kuusamo |
geographic_facet |
Kuusamo |
genre |
karelia* karelian |
genre_facet |
karelia* karelian |
op_source |
Geochemistry, Geophysics, Geosystems, 23 (8) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2021GC010324 info:eu-repo/semantics/altIdentifier/wos/000838102300001 info:eu-repo/grantAgreement/SNF/Ambizione/180126 http://hdl.handle.net/20.500.11850/565143 doi:10.3929/ethz-b-000565143 |
op_rights |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/20.500.11850/565143 https://doi.org/10.3929/ethz-b-000565143 https://doi.org/10.1029/2021GC010324 |
_version_ |
1766052856605966336 |