Metal-rich Scales in the Reykjanes Geothermal System, SW Iceland: Sulfide Minerals in a Seawater-dominated Hydrothermal Environment
Downhole sampling of unboiled liquid at 1350 and 1500 m depth in the seawater-dominated Reykjanes high-temperature geothermal system in Iceland shows that metal concentrations measured at surface are minimum values due to mineral precipitation in the wells; by analogy of similar tectonic setting, ho...
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| Language: | en |
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Université d'Ottawa / University of Ottawa
2011
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| Online Access: | http://hdl.handle.net/10393/19925 http://dx.doi.org/10.20381/ruor-4543 |