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The geochemistry of trace elements in geothermal fluids, Iceland
Nordic Volcanological Center, University of Iceland, Institute of Earth Sciences.ORCID iD: 0000-0003-3382-1764
Institute of Earth Sciences, University of Iceland.
Nagra.
Institute of Earth Sciences, University of Iceland.
2015 (English)In: Applied Geochemistry, ISSN 0883-2927, E-ISSN 1872-9134, Vol. 62, p. 207-223Article in journal (Refereed) Published
Abstract [en]

Trace element geochemistry was studied in geothermal fluids in Iceland. The major and trace element compositions of hot springs, sub-boiling, and two-phase (liquid and vapor) wells from 10 geothermal areas were used to reconstruct the fluid composition in the aquifers at depth. Aquifer fluid temperatures ranged from 4 to 300 °C, pH values between 4.5 and 9.3, and fluids typically contained total dissolved solids

Place, publisher, year, edition, pages
2015. Vol. 62, p. 207-223
National Category
Geochemistry
Research subject
Applied Geochemistry
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URN: urn:nbn:se:ltu:diva-5000DOI: 10.1016/j.apgeochem.2015.02.003Scopus ID: 2-s2.0-84943661184Local ID: 3034d193-a6ca-468d-ba31-f1499376c86fOAI: oai:DiVA.org:ltu-5000DiVA, id: diva2:977874
Note

Upprättat; 2015; 20160205 (hankas)

Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2019-04-30Bibliographically approved

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Kaasalainen, Hanna

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