Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions
Fluid inclusion evidence from the Grey River Tungsten Prospect, Newfoundland, and other tungsten deposits indicates that CO 2 is an important component of the hydrothermal fluid. Carbon dioxide is enriched in fluids evolved from granitic melts under high fluid pressure, while lower pressure fluids a...
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Canadian Science Publishing
1980
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Online Access: | http://dx.doi.org/10.1139/e80-082 http://www.nrcresearchpress.com/doi/pdf/10.1139/e80-082 |
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crcansciencepubl:10.1139/e80-082 2024-05-19T07:44:15+00:00 Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions Higgins, N. C. 1980 http://dx.doi.org/10.1139/e80-082 http://www.nrcresearchpress.com/doi/pdf/10.1139/e80-082 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 17, issue 7, page 823-830 ISSN 0008-4077 1480-3313 journal-article 1980 crcansciencepubl https://doi.org/10.1139/e80-082 2024-05-02T06:51:25Z Fluid inclusion evidence from the Grey River Tungsten Prospect, Newfoundland, and other tungsten deposits indicates that CO 2 is an important component of the hydrothermal fluid. Carbon dioxide is enriched in fluids evolved from granitic melts under high fluid pressure, while lower pressure fluids are chloride-rich. The association of tungsten deposits with these carbon dioxide rich hydrothermal fluids suggests that carbonate/bicarbonate complexes may be important in tungsten transport at very high fluid pressures. Article in Journal/Newspaper Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 17 7 823 830 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
language |
English |
description |
Fluid inclusion evidence from the Grey River Tungsten Prospect, Newfoundland, and other tungsten deposits indicates that CO 2 is an important component of the hydrothermal fluid. Carbon dioxide is enriched in fluids evolved from granitic melts under high fluid pressure, while lower pressure fluids are chloride-rich. The association of tungsten deposits with these carbon dioxide rich hydrothermal fluids suggests that carbonate/bicarbonate complexes may be important in tungsten transport at very high fluid pressures. |
format |
Article in Journal/Newspaper |
author |
Higgins, N. C. |
spellingShingle |
Higgins, N. C. Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions |
author_facet |
Higgins, N. C. |
author_sort |
Higgins, N. C. |
title |
Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions |
title_short |
Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions |
title_full |
Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions |
title_fullStr |
Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions |
title_full_unstemmed |
Fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions |
title_sort |
fluid inclusion evidence for the transport of tungsten by carbonate complexes in hydrothermal solutions |
publisher |
Canadian Science Publishing |
publishDate |
1980 |
url |
http://dx.doi.org/10.1139/e80-082 http://www.nrcresearchpress.com/doi/pdf/10.1139/e80-082 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Canadian Journal of Earth Sciences volume 17, issue 7, page 823-830 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e80-082 |
container_title |
Canadian Journal of Earth Sciences |
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17 |
container_issue |
7 |
container_start_page |
823 |
op_container_end_page |
830 |
_version_ |
1799484010743726080 |