A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity
Ten sphalerite separates isolated from mineralized samples in proximal and distal positions relative to the proposed main feeder fault systems at the Laisvall deposit were used to obtain an absolute age determina- tion of this world-class Pb-Zn deposit hosted by autochthonous Ediacaran to Lower Camb...
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ftunivgeneve:oai:unige.ch:unige:75497 2023-05-15T17:45:07+02:00 A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity Saintilan, Nicolas Schneider, Jens Stephens, Michael B. Chiaradia, Massimo Kouzmanov, Kalin Wälle, Marküs Fontboté, Lluís 2015 https://archive-ouverte.unige.ch/unige:75497 eng eng info:eu-repo/semantics/altIdentifier/doi/10.2113/econgeo.110.7.1779 unige:75497 https://archive-ouverte.unige.ch/unige:75497 info:eu-repo/semantics/restrictedAccess ISSN: 0361-0128 Economic geology and the bulletin of the Society of Economic Geologists, Vol. 110 (2015) pp. 1779-1801 info:eu-repo/classification/ddc/550 Text Article scientifique info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftunivgeneve https://doi.org/10.2113/econgeo.110.7.1779 2022-06-19T23:40:00Z Ten sphalerite separates isolated from mineralized samples in proximal and distal positions relative to the proposed main feeder fault systems at the Laisvall deposit were used to obtain an absolute age determina- tion of this world-class Pb-Zn deposit hosted by autochthonous Ediacaran to Lower Cambrian sandstone and located currently along the erosional front of the Scandinavian Caledonides in northern Sweden. Residue and leachate fractions of each separate were obtained using the crush-leaching technique. All samples correspond to sphalerite formed using reduced sulfur derived from thermochemical sulfate reduction, three of them from disseminated ore in the Lower Sandstone, two from the disseminated ore in the Upper Sandstone, and five from steeply dipping galena-sphalerite-calcite veinlets interpreted in previous works as remobilization of dis- seminated ores. The isotope dilution-thermal ionization mass spectrometry (ID-TIMS) data yield an overall complex Rb-Sr isotope pattern with two distinct trends in the 87Sr/86Sr vs. 87Rb/86Sr isochron diagram. The three sphalerite residues of disseminated mineralization from the Lower Sandstone orebody show Rb-Sr isotope sys- tematics indicative of undisturbed primary precipitates, and yield an isochron model age of 467 ± 5 Ma (mean square weighted deviation, MSWD, 1.4). Since the isochron is based on three points, the obtained age is to be considered as preliminary. Yet, the obtained age is fully consistent with geologic evidence reported by previous authors and pointing to Middle Ordovician timing of ore formation. The ID-TIMS data were complemented by laser ablation-inductively coupled plasma mass spectrometry (LA-ICPMS) analyses on the same sphalerite samples. The data support the hypothesis that the measured ID-TIMS Rb and Sr contents in these sphalerite residues are held in the sphalerite structure itself and are not related to micro-inclusions. The most viable hypothesis, in agreement with published work, is that during rapid growth, sphalerite may incorporate ... Article in Journal/Newspaper Northern Sweden Université de Genève: Archive ouverte UNIGE Laisvall ENVELOPE(17.167,17.167,66.133,66.133) Economic Geology 110 7 1779 1801 |
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Université de Genève: Archive ouverte UNIGE |
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English |
topic |
info:eu-repo/classification/ddc/550 |
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info:eu-repo/classification/ddc/550 Saintilan, Nicolas Schneider, Jens Stephens, Michael B. Chiaradia, Massimo Kouzmanov, Kalin Wälle, Marküs Fontboté, Lluís A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity |
topic_facet |
info:eu-repo/classification/ddc/550 |
description |
Ten sphalerite separates isolated from mineralized samples in proximal and distal positions relative to the proposed main feeder fault systems at the Laisvall deposit were used to obtain an absolute age determina- tion of this world-class Pb-Zn deposit hosted by autochthonous Ediacaran to Lower Cambrian sandstone and located currently along the erosional front of the Scandinavian Caledonides in northern Sweden. Residue and leachate fractions of each separate were obtained using the crush-leaching technique. All samples correspond to sphalerite formed using reduced sulfur derived from thermochemical sulfate reduction, three of them from disseminated ore in the Lower Sandstone, two from the disseminated ore in the Upper Sandstone, and five from steeply dipping galena-sphalerite-calcite veinlets interpreted in previous works as remobilization of dis- seminated ores. The isotope dilution-thermal ionization mass spectrometry (ID-TIMS) data yield an overall complex Rb-Sr isotope pattern with two distinct trends in the 87Sr/86Sr vs. 87Rb/86Sr isochron diagram. The three sphalerite residues of disseminated mineralization from the Lower Sandstone orebody show Rb-Sr isotope sys- tematics indicative of undisturbed primary precipitates, and yield an isochron model age of 467 ± 5 Ma (mean square weighted deviation, MSWD, 1.4). Since the isochron is based on three points, the obtained age is to be considered as preliminary. Yet, the obtained age is fully consistent with geologic evidence reported by previous authors and pointing to Middle Ordovician timing of ore formation. The ID-TIMS data were complemented by laser ablation-inductively coupled plasma mass spectrometry (LA-ICPMS) analyses on the same sphalerite samples. The data support the hypothesis that the measured ID-TIMS Rb and Sr contents in these sphalerite residues are held in the sphalerite structure itself and are not related to micro-inclusions. The most viable hypothesis, in agreement with published work, is that during rapid growth, sphalerite may incorporate ... |
format |
Article in Journal/Newspaper |
author |
Saintilan, Nicolas Schneider, Jens Stephens, Michael B. Chiaradia, Massimo Kouzmanov, Kalin Wälle, Marküs Fontboté, Lluís |
author_facet |
Saintilan, Nicolas Schneider, Jens Stephens, Michael B. Chiaradia, Massimo Kouzmanov, Kalin Wälle, Marküs Fontboté, Lluís |
author_sort |
Saintilan, Nicolas |
title |
A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity |
title_short |
A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity |
title_full |
A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity |
title_fullStr |
A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity |
title_full_unstemmed |
A Middle Ordovician age for the Laisvall sandstone-hosted Pb-Zn deposit, Sweden: A response to early Caledonian orogenic activity |
title_sort |
middle ordovician age for the laisvall sandstone-hosted pb-zn deposit, sweden: a response to early caledonian orogenic activity |
publishDate |
2015 |
url |
https://archive-ouverte.unige.ch/unige:75497 |
long_lat |
ENVELOPE(17.167,17.167,66.133,66.133) |
geographic |
Laisvall |
geographic_facet |
Laisvall |
genre |
Northern Sweden |
genre_facet |
Northern Sweden |
op_source |
ISSN: 0361-0128 Economic geology and the bulletin of the Society of Economic Geologists, Vol. 110 (2015) pp. 1779-1801 |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.2113/econgeo.110.7.1779 unige:75497 https://archive-ouverte.unige.ch/unige:75497 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.2113/econgeo.110.7.1779 |
container_title |
Economic Geology |
container_volume |
110 |
container_issue |
7 |
container_start_page |
1779 |
op_container_end_page |
1801 |
_version_ |
1766147869650190336 |