Soil CO2 emission and stable isotopes (δ13C, δ18O) of CO2 and calcites reveal the fluid origin and thermal energy in the supercritical geothermal system of Krafla, Iceland-Reference-Cited by-同舟云学术

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Soil CO2 emission and stable isotopes (δ13C, δ18O) of CO2 and calcites reveal the fluid origin and thermal energy in the supercritical geothermal system of Krafla, Iceland

Published:2024-03 Issue: Volume:447 Page:108032
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Bini Giulio,Chiodini Giovanni,Ricci Tullio,Sciarra Alessandra,Caliro Stefano,Mortensen Anette K.,Martini Marco,Mitchell Andrew,Santi Alessandro,Costa Antonio

Funder

MIUR

Horizon 2020

Ministero dell’Istruzione, dell’Università e della Ricerca

Publisher

Elsevier BV

Reference81 articles.

1. Öxarfjördur. Studies of Gas. Orkustofnun OS-98051;Ármannsson,1998

2. Gas changes in the Krafla geothermal system, Iceland;Ármannsson;Chem. Geol.,1989

3. CO2 budget of the Krafla geothermal system, NE-Iceland;Ármannsson,2007

4. New Conceptual Model for the Magma-Hydrothermal-Tectonic System of Krafla, NE Iceland;Árnason;Geosciences,2020

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