Abstract Details
(2020) The Surtsey Volcano Geothermal System: An Analogue to Constrain Elemental Cycling in Seamounts?
Kleine BI, Stefánsson A, Kjartansdóttir R, Prause S, Weisenberger TB, Sveinbjörnsdóttir ÁE, Jackson M & Gudmundsson MT
https://doi.org/10.46427/gold2020.1333
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14e: Plenary Hall, Wednesday 24th June 06:45 - 06:48
Barbara Irene Kleine
View abstracts at 3 conferences in series
Andri Stefánsson View all 3 abstracts at Goldschmidt2020
Ríkey Kjartansdóttir View abstracts at 6 conferences in series
Simon Prause View all 3 abstracts at Goldschmidt2020 View abstracts at 3 conferences in series
Tobias Björn Weisenberger View all 4 abstracts at Goldschmidt2020 View abstracts at 2 conferences in series
Árný Erla Sveinbjörnsdóttir View abstracts at 2 conferences in series
Marie Jackson View abstracts at 2 conferences in series
Magnús Tumi Gudmundsson View all 2 abstracts at Goldschmidt2020
Andri Stefánsson View all 3 abstracts at Goldschmidt2020
Ríkey Kjartansdóttir View abstracts at 6 conferences in series
Simon Prause View all 3 abstracts at Goldschmidt2020 View abstracts at 3 conferences in series
Tobias Björn Weisenberger View all 4 abstracts at Goldschmidt2020 View abstracts at 2 conferences in series
Árný Erla Sveinbjörnsdóttir View abstracts at 2 conferences in series
Marie Jackson View abstracts at 2 conferences in series
Magnús Tumi Gudmundsson View all 2 abstracts at Goldschmidt2020
Listed below are questions that have been submitted by the community that the author will try and cover in their presentation. To submit a question, ensure you are signed in to the website. Authors or session conveners approve questions before they are displayed here.
Submitted by Benjamin Tutolo on Tuesday 23rd June 04:46
It's interestesing and important that your study shows the significant importance of these low-temperature hydrothermal systemts for global geochemical fluxes. Do you think that there is a higher temperature component of hydrothermal fluxes in seamounts? If so, when?
It's interestesing and important that your study shows the significant importance of these low-temperature hydrothermal systemts for global geochemical fluxes. Do you think that there is a higher temperature component of hydrothermal fluxes in seamounts? If so, when?
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