Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia
Trace element composition (Zn, Pb, In, Cd, Ag, As, Sb, Se, Te, Mo, Sn, Ru, Rh, Os, Ir, and Pt) of sulfide inclusions in garnets was studied with a proton microprobe HIAF. The PGE contents of sulfides are 15-300 chondrite values. This is several times lower than that of sulfide globules from olivines...
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ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/773589a5-24c3-410b-bf76-02cb8451d3bc 2023-05-15T18:44:54+02:00 Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia Barashkov, Yu P. Griffin, W. L. Tel'nikova, S. B. 1998 https://researchers.mq.edu.au/en/publications/773589a5-24c3-410b-bf76-02cb8451d3bc http://www.scopus.com/inward/record.url?scp=0347704484&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Barashkov , Y P , Griffin , W L & Tel'nikova , S B 1998 , ' Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia ' , Geochemistry International , vol. 36 , no. 12 , pp. 1147-1153 . article 1998 ftmacquarieunicr 2022-11-06T06:34:54Z Trace element composition (Zn, Pb, In, Cd, Ag, As, Sb, Se, Te, Mo, Sn, Ru, Rh, Os, Ir, and Pt) of sulfide inclusions in garnets was studied with a proton microprobe HIAF. The PGE contents of sulfides are 15-300 chondrite values. This is several times lower than that of sulfide globules from olivines and diamonds. The sulfides have similar chondrite-normalized PGE patterns with a clearly pronounced Ru minimum which is not typical of sulfides from diamonds and olivines. Article in Journal/Newspaper Yakutia Macquarie University Research Portal |
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Open Polar |
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Macquarie University Research Portal |
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ftmacquarieunicr |
language |
English |
description |
Trace element composition (Zn, Pb, In, Cd, Ag, As, Sb, Se, Te, Mo, Sn, Ru, Rh, Os, Ir, and Pt) of sulfide inclusions in garnets was studied with a proton microprobe HIAF. The PGE contents of sulfides are 15-300 chondrite values. This is several times lower than that of sulfide globules from olivines and diamonds. The sulfides have similar chondrite-normalized PGE patterns with a clearly pronounced Ru minimum which is not typical of sulfides from diamonds and olivines. |
format |
Article in Journal/Newspaper |
author |
Barashkov, Yu P. Griffin, W. L. Tel'nikova, S. B. |
spellingShingle |
Barashkov, Yu P. Griffin, W. L. Tel'nikova, S. B. Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia |
author_facet |
Barashkov, Yu P. Griffin, W. L. Tel'nikova, S. B. |
author_sort |
Barashkov, Yu P. |
title |
Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia |
title_short |
Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia |
title_full |
Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia |
title_fullStr |
Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia |
title_full_unstemmed |
Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia |
title_sort |
trace element composition of sulfide inclusions in garnets from the udachnaya kimberlite pipe, yakutia |
publishDate |
1998 |
url |
https://researchers.mq.edu.au/en/publications/773589a5-24c3-410b-bf76-02cb8451d3bc http://www.scopus.com/inward/record.url?scp=0347704484&partnerID=8YFLogxK |
genre |
Yakutia |
genre_facet |
Yakutia |
op_source |
Barashkov , Y P , Griffin , W L & Tel'nikova , S B 1998 , ' Trace element composition of sulfide inclusions in garnets from the Udachnaya Kimberlite Pipe, Yakutia ' , Geochemistry International , vol. 36 , no. 12 , pp. 1147-1153 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1766235755932286976 |