LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield

Gold concentrations in Bi-chalcogenides (tellurobismuthite and laitakarite) from four deposits in the Fennoscandian Shield have been determined by LA-ICP-MS. Both minerals contain gold above background levels, with tellurobismuthite from Orivesi (Kutamejärvi), Finland, with concentrations between 1...

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Main Authors: Cook, N., Ciobanu, C., Danushevskiy, L.
Format: Article in Journal/Newspaper
Language:English
Published: Geologian Tutkimuskeskus 2007
Subjects:
Online Access:http://hdl.handle.net/2440/46565
id ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/46565
record_format openpolar
spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/46565 2023-05-15T16:12:54+02:00 LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield Cook, N. Ciobanu, C. Danushevskiy, L. 2007 http://hdl.handle.net/2440/46565 en eng Geologian Tutkimuskeskus Geologian Tutkimuskeskus. Opas, 2007; 53:23-30 0781-643X http://hdl.handle.net/2440/46565 Cook, N. [0000-0002-7470-3935] http://arkisto.gtk.fi/op/op53.pdf gold ores tellurobismuthite laitakarite gold laser ablation ICP mass spectra Orivesi Orijärvi Finland Glava Sweden Moberg Norway Journal article 2007 ftunivadelaidedl 2023-02-06T07:06:33Z Gold concentrations in Bi-chalcogenides (tellurobismuthite and laitakarite) from four deposits in the Fennoscandian Shield have been determined by LA-ICP-MS. Both minerals contain gold above background levels, with tellurobismuthite from Orivesi (Kutamejärvi), Finland, with concentrations between 1 and more than 300 ppm. The concentrations of gold vary over two orders of magnitude within individual analysed patches. The gold signal in the majority of individual LA-ICP-MS profiles is irregular. Laitakarite from Orijärvi (Finland) contains lesser concentrations (up to 10 ppm). Tellurobismuthite in two Sveconorwegian orogenic gold occurrences differ markedly; 798 and 2,472 ppm in Glava (Sweden) and <1 ppm at Moberg (Norway). The present dataset shows that Bi-chalcogenides may, in some cases, be considered as gold carriers, and can contain gold at similar levels as pyrite. Measured concentrations in tellurobismuthite are, with the exception of Glava, lower than those obtained in published experimental work on that mineral. This is interpreted as due to the formation of discrete sub-????m sized inclusions of gold within the Bi-minerals during post-depositional overprinting. The influence of metamorphism is clearly an important factor in determining the distribution of gold within Bi-chalcogenides. Nigel J. Cook, Cristiana L. Ciobanu and Leonid Danushevskiy Article in Journal/Newspaper Fennoscandian The University of Adelaide: Digital Library Moberg ENVELOPE(20.782,20.782,69.518,69.518) Norway
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
topic gold ores
tellurobismuthite
laitakarite
gold
laser ablation
ICP mass spectra
Orivesi
Orijärvi
Finland
Glava
Sweden
Moberg
Norway
spellingShingle gold ores
tellurobismuthite
laitakarite
gold
laser ablation
ICP mass spectra
Orivesi
Orijärvi
Finland
Glava
Sweden
Moberg
Norway
Cook, N.
Ciobanu, C.
Danushevskiy, L.
LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield
topic_facet gold ores
tellurobismuthite
laitakarite
gold
laser ablation
ICP mass spectra
Orivesi
Orijärvi
Finland
Glava
Sweden
Moberg
Norway
description Gold concentrations in Bi-chalcogenides (tellurobismuthite and laitakarite) from four deposits in the Fennoscandian Shield have been determined by LA-ICP-MS. Both minerals contain gold above background levels, with tellurobismuthite from Orivesi (Kutamejärvi), Finland, with concentrations between 1 and more than 300 ppm. The concentrations of gold vary over two orders of magnitude within individual analysed patches. The gold signal in the majority of individual LA-ICP-MS profiles is irregular. Laitakarite from Orijärvi (Finland) contains lesser concentrations (up to 10 ppm). Tellurobismuthite in two Sveconorwegian orogenic gold occurrences differ markedly; 798 and 2,472 ppm in Glava (Sweden) and <1 ppm at Moberg (Norway). The present dataset shows that Bi-chalcogenides may, in some cases, be considered as gold carriers, and can contain gold at similar levels as pyrite. Measured concentrations in tellurobismuthite are, with the exception of Glava, lower than those obtained in published experimental work on that mineral. This is interpreted as due to the formation of discrete sub-????m sized inclusions of gold within the Bi-minerals during post-depositional overprinting. The influence of metamorphism is clearly an important factor in determining the distribution of gold within Bi-chalcogenides. Nigel J. Cook, Cristiana L. Ciobanu and Leonid Danushevskiy
format Article in Journal/Newspaper
author Cook, N.
Ciobanu, C.
Danushevskiy, L.
author_facet Cook, N.
Ciobanu, C.
Danushevskiy, L.
author_sort Cook, N.
title LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield
title_short LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield
title_full LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield
title_fullStr LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield
title_full_unstemmed LA-ICP-MS determination of gold in Bi-chalcogenides from four deposits in the Fennoscandian Shield
title_sort la-icp-ms determination of gold in bi-chalcogenides from four deposits in the fennoscandian shield
publisher Geologian Tutkimuskeskus
publishDate 2007
url http://hdl.handle.net/2440/46565
long_lat ENVELOPE(20.782,20.782,69.518,69.518)
geographic Moberg
Norway
geographic_facet Moberg
Norway
genre Fennoscandian
genre_facet Fennoscandian
op_source http://arkisto.gtk.fi/op/op53.pdf
op_relation Geologian Tutkimuskeskus. Opas, 2007; 53:23-30
0781-643X
http://hdl.handle.net/2440/46565
Cook, N. [0000-0002-7470-3935]
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