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Solubility of uranium in hydrothermal fluids at 25°-300°: Implications for the formation of uranium deposits

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Created 13/01/2025

Updated 13/01/2025

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The present report provides a compilation of thermodynamic data for geologically relevant uranium species suitable for geochemical equilibrium calculations from low to moderate temperatures (up to 300°C). It also reports a set of diagrams displaying the solubility of key uranium ore minerals (uraninite, coffinite and carnotite) and the stability of uranium and vanadium complexes at temperatures between 25° and 300°C. Further, it discusses mass-balance calculations of fluid-rock reactions at temperatures up to 200°C relevant to understanding the behaviour of uranium in unconformity-related uranium and sediment-hosted stratiform copper-uranium deposits.

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Title Solubility of uranium in hydrothermal fluids at 25°-300°: Implications for the formation of uranium deposits
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/bebd38dc-e5ab-432d-8a89-97532d615912
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage http://www.ga.gov.au/place-names/PlaceDetails.jsp?submit1=GA1
Data Portal data.gov.au

Data Source

This dataset was originally found on data.gov.au "Solubility of uranium in hydrothermal fluids at 25°-300°: Implications for the formation of uranium deposits". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/solubility-of-uranium-in-hydrothermal-fluids-at-25a-300a-implications-for-the-formation-of-uran

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