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...
Published in: | GFF |
---|---|
Main Authors: | , , |
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 |
_version_ | 1821510780233711616 |
---|---|
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 |
id | ftluleatu:oai:DiVA.org:ltu-93416 |
institution | Open Polar |
language | English |
op_collection_id | ftluleatu |
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 |
publishDate | 2022 |
publisher | Luleå tekniska universitet, Geovetenskap och miljöteknik |
record_format | openpolar |
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 |