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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Published in:Canadian Journal of Earth Sciences
Main Author: Higgins, N. C.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1980
Subjects:
Online Access:http://dx.doi.org/10.1139/e80-082
http://www.nrcresearchpress.com/doi/pdf/10.1139/e80-082
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spelling 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
institution Open Polar
collection Canadian Science Publishing
op_collection_id 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
container_volume 17
container_issue 7
container_start_page 823
op_container_end_page 830
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