Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden

The Svärdsjö Zn-Pb-Cu deposit is situated in the heavily mineralised Bergslagen lithotectonic unit of the Fennoscandian shield, south-central Sweden. Intense hydrothermal alteration followed by a strong overprint by deformation and metamorphism during the Svecokarelian orogeny complicate interpretat...

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Published in:GFF
Main Authors: Fahlvik, Anton, Kampmann, Tobias Christoph, Jansson, Nils F.
Format: Article in Journal/Newspaper
Language:English
Published: Luleå tekniska universitet, Geovetenskap och miljöteknik 2022
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-93416
https://doi.org/10.1080/11035897.2022.2120065
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author Fahlvik, Anton
Kampmann, Tobias Christoph
Jansson, Nils F.
author_facet Fahlvik, Anton
Kampmann, Tobias Christoph
Jansson, Nils F.
author_sort Fahlvik, Anton
collection Luleå University of Technology Publications (DiVA)
container_start_page 1
container_title GFF
description The Svärdsjö Zn-Pb-Cu deposit is situated in the heavily mineralised Bergslagen lithotectonic unit of the Fennoscandian shield, south-central Sweden. Intense hydrothermal alteration followed by a strong overprint by deformation and metamorphism during the Svecokarelian orogeny complicate interpretation of the local geology. Integration of whole-rock lithogeochemical and petrographic methods has allowed the mainly dacitic volcanic host succession and effects of ore-related hydrothermal alteration to be characterised. Mineralisation is hosted by 2–15 m thick, commonly skarn-altered dolomitic marble interbeds. Zones of strong–intense hydrothermal chlorite-sericite alteration envelop the marble units, recording mass gains of Fe and Mg, as well as Na depletion. Minerals such as cordierite, anthophyllite and sillimanite formed in these rocks during regional metamorphism. Mineralisation via sub-seafloor replacement is suggested for the deposit based on alteration zoning and the irregular, stratabound, marble-hosted style of sulphide lenses. It is inferred that mineralisation formed via neutralisation of hot, acidic metalliferous fluids. Geochemically and lithologically distinct units adjacent to the mineralised zones can serve as marker units to aid further exploration in the area. Mass change calculations reveal that Fe and Mg enrichment, as well as Na depletion exhibit detectable changes extending up to 100 m from the mineralised lenses, providing exploration vectors. Validerad;2023;Nivå 2;2023-12-05 (hanlid); Funder: Boliden Mineral AB; Full text license: CC BY-NC-ND
format Article in Journal/Newspaper
genre Fennoscandian
genre_facet Fennoscandian
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language English
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op_container_end_page 19
op_doi https://doi.org/10.1080/11035897.2022.2120065
op_relation GFF, 1103-5897, 2022, 144:3-4, s. 177-195
doi:10.1080/11035897.2022.2120065
ISI:000863647200001
op_rights info:eu-repo/semantics/openAccess
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publisher Luleå tekniska universitet, Geovetenskap och miljöteknik
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spelling ftluleatu:oai:DiVA.org:ltu-93416 2025-01-16T21:51:55+00:00 Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden Fahlvik, Anton Kampmann, Tobias Christoph Jansson, Nils F. 2022 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-93416 https://doi.org/10.1080/11035897.2022.2120065 eng eng Luleå tekniska universitet, Geovetenskap och miljöteknik Exploration Department, Boliden Mineral, Boliden, Sweden GFF, 1103-5897, 2022, 144:3-4, s. 177-195 doi:10.1080/11035897.2022.2120065 ISI:000863647200001 info:eu-repo/semantics/openAccess Lithogeochemistry Bergslagen alteration massive sulphides Skarn VMS Geology Geologi Article in journal info:eu-repo/semantics/article text 2022 ftluleatu https://doi.org/10.1080/11035897.2022.2120065 2024-12-18T12:24:46Z The Svärdsjö Zn-Pb-Cu deposit is situated in the heavily mineralised Bergslagen lithotectonic unit of the Fennoscandian shield, south-central Sweden. Intense hydrothermal alteration followed by a strong overprint by deformation and metamorphism during the Svecokarelian orogeny complicate interpretation of the local geology. Integration of whole-rock lithogeochemical and petrographic methods has allowed the mainly dacitic volcanic host succession and effects of ore-related hydrothermal alteration to be characterised. Mineralisation is hosted by 2–15 m thick, commonly skarn-altered dolomitic marble interbeds. Zones of strong–intense hydrothermal chlorite-sericite alteration envelop the marble units, recording mass gains of Fe and Mg, as well as Na depletion. Minerals such as cordierite, anthophyllite and sillimanite formed in these rocks during regional metamorphism. Mineralisation via sub-seafloor replacement is suggested for the deposit based on alteration zoning and the irregular, stratabound, marble-hosted style of sulphide lenses. It is inferred that mineralisation formed via neutralisation of hot, acidic metalliferous fluids. Geochemically and lithologically distinct units adjacent to the mineralised zones can serve as marker units to aid further exploration in the area. Mass change calculations reveal that Fe and Mg enrichment, as well as Na depletion exhibit detectable changes extending up to 100 m from the mineralised lenses, providing exploration vectors. Validerad;2023;Nivå 2;2023-12-05 (hanlid); Funder: Boliden Mineral AB; Full text license: CC BY-NC-ND Article in Journal/Newspaper Fennoscandian Luleå University of Technology Publications (DiVA) GFF 1 19
spellingShingle Lithogeochemistry
Bergslagen
alteration
massive sulphides
Skarn
VMS
Geology
Geologi
Fahlvik, Anton
Kampmann, Tobias Christoph
Jansson, Nils F.
Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden
title Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden
title_full Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden
title_fullStr Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden
title_full_unstemmed Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden
title_short Hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the Svärdsjö Zn-Pb-Cu deposit, Bergslagen, Sweden
title_sort hydrothermal alteration, lithogeochemical marker units and vectors towards mineralisation at the svärdsjö zn-pb-cu deposit, bergslagen, sweden
topic Lithogeochemistry
Bergslagen
alteration
massive sulphides
Skarn
VMS
Geology
Geologi
topic_facet Lithogeochemistry
Bergslagen
alteration
massive sulphides
Skarn
VMS
Geology
Geologi
url http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-93416
https://doi.org/10.1080/11035897.2022.2120065