Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden
The Paleoproterozoic Falun Zn-Pb-Cu-(Au-Ag) pyritic sulfide deposit in the Bergslagen ore district, Sweden, is enveloped by hydrothermally altered rocks metamorphosed to the lower amphibolite facies. Immobile-element ratios suggest that the alteration precursors were volcanic rocks of mainly rhyolit...
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Uppsala universitet, Mineralogi, petrologi och tektonik
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ftuppsalauniv:oai:DiVA.org:uu-351037 2023-05-15T16:13:07+02:00 Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden Kampmann, Tobias C. Jansson, Nils F. Stephens, Michael B. Majka, Jaroslaw Lasskogen, Jonas 2017 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-351037 https://doi.org/10.5382/econgeo.2017.4504 eng eng Uppsala universitet, Mineralogi, petrologi och tektonik Luleå Univ Technol, Div Geosci & Environm Engn, SE-97187 Lulea, Sweden. Luleå Univ Technol, Div Geosci & Environm Engn, SE-97187 Lulea, Sweden.;Geol Survey Sweden, Box 670, SE-75128 Uppsala, Sweden. AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Al Mickiewicza 30, PL-30059 Krakow, Poland. Boliden Mineral, Explorat Dept, Boliden, Sweden. SOC ECONOMIC GEOLOGISTS, INC Economic geology and the bulletin of the Society of Economic Geologists, 0361-0128, 2017, 112:5, s. 1111-1152 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-351037 doi:10.5382/econgeo.2017.4504 ISI:000426874300005 info:eu-repo/semantics/openAccess Geology Geologi Article in journal info:eu-repo/semantics/article text 2017 ftuppsalauniv https://doi.org/10.5382/econgeo.2017.4504 2023-02-23T21:47:31Z The Paleoproterozoic Falun Zn-Pb-Cu-(Au-Ag) pyritic sulfide deposit in the Bergslagen ore district, Sweden, is enveloped by hydrothermally altered rocks metamorphosed to the lower amphibolite facies. Immobile-element ratios suggest that the alteration precursors were volcanic rocks of mainly rhyolitic to dacitic composition. Least altered examples of these rocks plot along magmatic fractionation trends outlined by late-to post-ore feldsparphyric metadacite dikes and post-ore granitoid plutons, consistent with a comagmatic relationship between these calc-alkaline, coeval (<10-m.y.) suites. Dolomite or calcite marble, as well as diopside-hedenbergite or tremolite skarn, form subordinate but important lithologic components in the hydrothermally altered zone. Marble occurs as fragments in the massive pyritic sulfide mineralization, suggesting that at least some mineralization formed by carbonate replacement. Mass-change calculations suggest that the hydrothermally altered volcanic rocks gained Mg and Fe and generally lost Ca, K, and Na. Proximal, quartz-anthophyllite-rich altered rocks additionally gained Si, whereas several types of biotite-rich altered rocks lost this element. These mass changes along with mineral chemical data for anthophyllite, biotite, cordierite, and garnet, and the common occurrence of quartz indicate that chloritization, sericitization, and silicification were the dominant premetamorphic alteration styles. A zonation from distal sericitized and silicified volcanic rocks to intermediate sericitized rocks, partly overprinted by chloritization (Mg-rich chlorite), and proximal siliceous and intensely chloritized (Fe-rich chlorite) rocks has been identified. Furthermore, mass changes in more peripheral parts of the altered zone toward the southeast of the deposit suggest that the alteration weakens gradationally toward the volcanic and subvolcanic rocks surrounding the deposit. These patterns represent vectors toward mineralization. Intensely chloritized rocks, largely represented by a single, ... Article in Journal/Newspaper Fennoscandian Uppsala University: Publications (DiVA) Economic Geology 112 5 1111 1152 |
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Geology Geologi Kampmann, Tobias C. Jansson, Nils F. Stephens, Michael B. Majka, Jaroslaw Lasskogen, Jonas Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden |
topic_facet |
Geology Geologi |
description |
The Paleoproterozoic Falun Zn-Pb-Cu-(Au-Ag) pyritic sulfide deposit in the Bergslagen ore district, Sweden, is enveloped by hydrothermally altered rocks metamorphosed to the lower amphibolite facies. Immobile-element ratios suggest that the alteration precursors were volcanic rocks of mainly rhyolitic to dacitic composition. Least altered examples of these rocks plot along magmatic fractionation trends outlined by late-to post-ore feldsparphyric metadacite dikes and post-ore granitoid plutons, consistent with a comagmatic relationship between these calc-alkaline, coeval (<10-m.y.) suites. Dolomite or calcite marble, as well as diopside-hedenbergite or tremolite skarn, form subordinate but important lithologic components in the hydrothermally altered zone. Marble occurs as fragments in the massive pyritic sulfide mineralization, suggesting that at least some mineralization formed by carbonate replacement. Mass-change calculations suggest that the hydrothermally altered volcanic rocks gained Mg and Fe and generally lost Ca, K, and Na. Proximal, quartz-anthophyllite-rich altered rocks additionally gained Si, whereas several types of biotite-rich altered rocks lost this element. These mass changes along with mineral chemical data for anthophyllite, biotite, cordierite, and garnet, and the common occurrence of quartz indicate that chloritization, sericitization, and silicification were the dominant premetamorphic alteration styles. A zonation from distal sericitized and silicified volcanic rocks to intermediate sericitized rocks, partly overprinted by chloritization (Mg-rich chlorite), and proximal siliceous and intensely chloritized (Fe-rich chlorite) rocks has been identified. Furthermore, mass changes in more peripheral parts of the altered zone toward the southeast of the deposit suggest that the alteration weakens gradationally toward the volcanic and subvolcanic rocks surrounding the deposit. These patterns represent vectors toward mineralization. Intensely chloritized rocks, largely represented by a single, ... |
format |
Article in Journal/Newspaper |
author |
Kampmann, Tobias C. Jansson, Nils F. Stephens, Michael B. Majka, Jaroslaw Lasskogen, Jonas |
author_facet |
Kampmann, Tobias C. Jansson, Nils F. Stephens, Michael B. Majka, Jaroslaw Lasskogen, Jonas |
author_sort |
Kampmann, Tobias C. |
title |
Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden |
title_short |
Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden |
title_full |
Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden |
title_fullStr |
Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden |
title_full_unstemmed |
Systematics of Hydrothermal Alteration at the Falun Base Metal Sulfide Deposit and Implications for Ore Genesis and Exploration, Bergslagen Ore District, Fennoscandian Shield, Sweden |
title_sort |
systematics of hydrothermal alteration at the falun base metal sulfide deposit and implications for ore genesis and exploration, bergslagen ore district, fennoscandian shield, sweden |
publisher |
Uppsala universitet, Mineralogi, petrologi och tektonik |
publishDate |
2017 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-351037 https://doi.org/10.5382/econgeo.2017.4504 |
genre |
Fennoscandian |
genre_facet |
Fennoscandian |
op_relation |
Economic geology and the bulletin of the Society of Economic Geologists, 0361-0128, 2017, 112:5, s. 1111-1152 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-351037 doi:10.5382/econgeo.2017.4504 ISI:000426874300005 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5382/econgeo.2017.4504 |
container_title |
Economic Geology |
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112 |
container_issue |
5 |
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1111 |
op_container_end_page |
1152 |
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1765998718826315776 |