Isotope systematics of Icelandic thermal fluids

TitleIsotope systematics of Icelandic thermal fluids
Publication TypeJournal Article
Year of Publication2017
AuthorsStefansson A., Hilton DR, Sveinbjornsdottir A.E, Torssander P., Heinemeier J., Barnes J.D, Ono S., Halldórsson S.A, Fiebig J., Arnorsson S.
JournalJournal of Volcanology and Geothermal Research
Volume337
Pagination146-164
Date Published2017/05
Type of ArticleReview
ISBN Number0377-0273
Accession NumberWOS:000402216600011
Keywordscarbon-isotope; divergent plate boundaries; eruption; Geothermal; helium-isotopes; Iceland; isotopes; lakagigar; mantle plume; Redox reactions; subglacial basalts; submarine hydrothermal vents; systems; Thermal fluids; trace-elements; volatiles
Abstract

Thermal fluids in Iceland range in temperature from <10 degrees C to >440 degrees C and are dominated by water (>97 mol%) with a chloride concentration from <10 ppm to >20,000 ppm. The isotope systematics of the fluids reveal many important features of the source(s) and transport properties of volatiles at this divergent plate boundary. Studies spanning over four decades have revealed a large range of values for delta D (-131 to +3.3%o), tritium (-0.4 to +13.8 TU), delta(18) O(-20.8 to + 2.3%o), He-3/He-4 (3.1 to 30.4 R-A), delta B-11 (-6.7 to+25.0%o), delta C-13 Sigma co(2) (-27.4 to+ 4.6%o), C-1 Sigma co(2), (+0.6 to + 118 pMC), delta C-l3(CH4) (-523 to-17.8%o), delta N-15 (-10.5 to+3.0%o), 8(34)C Sigma s(-ll) (-10.9 to (+)3.4%o), delta S-34(SO4) (-2.0to + 21.2%) and delta Cl-37 (-1.0 to + 2.1%o) in both liquid and vapor phases. Based on this isotopic dataset, the thermal waters originate from meteoric inputs and/or seawater. For other volatiles, degassing of mantle-derived melts contributes to He, CO2 and possibly also to Cl in the fluids. Water-basalt interaction also contributes to CO2 and is the major source of H2S, SO4, Cl and B in the fluids. Redox reactions additionally influence the composition of the fluids, for example, oxidation of H2S to SO4 and reduction of CO2 to CH4. Air water interaction mainly controls N-2, Ar and Ne concentrations. The large range of many non-reactive volatile isotope ratios, such as delta C-13 Sigma co(2)and(34)S Sigma S-u indicate heterogeneity of the mantle and mantle-derived melts beneath Iceland. In contrast, the large range of many reactive isotopes, such as delta C-13 Sigma co(2), and delta S-34 Sigma S-u, are heavily affected by processes occurring within the geothermal systems, including fluid-rock interaction, depressurization boiling, and isotopic fractionation between secondary minerals and the aqueous and vapor species. Variations due to these geothermal processes may exceed differences observed among various crust and mantle sources, highlighting the importance and effects of chemical reactions on the isotope systematics of reactive elements. (C) 2017 Elsevier B.V. All rights reserved.

DOI10.1016/j.jvolgeores.2017.02.006
Short TitleJ. Volcanol. Geotherm. Res.
Student Publication: 
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