Hydrothermal calcite formation in Campi Flegrei caldera, Italy: unraveling carbon sink processes in alkaline volcanic systems
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Publisher
Springer Science and Business Media LLC
Link
https://www.nature.com/articles/s41598-024-67746-8.pdf
Reference39 articles.
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2. Fischer, T. P. et al. The emissions of CO2 and other volatiles from the world’s subaerial volcanoes. Sci. Rep. 9, 18716. https://doi.org/10.1038/s41598-019-54682-1 (2019).
3. Werner, C., Fischer, T.P., Aiuppa, A., Edmonds, M., Cardellini, C., Carn, S., Chiodini, G., Cottrell, E., Burton, M., Shinohara, H. & Allard, P. Carbon dioxide emissions from subaerial volcanic regions: Two decades in review. In Deep Carbon; Past to Present (eds Orcutt, B.N., Daniel, I. & Dasgupta, R.) 188–236 (Cambridge University Press, 2019). https://doi.org/10.1017/9781108677950.008.
4. Chiodini, G. et al. Long-term variations of the Campi Flegrei, Italy, volcanic system as revealed by the monitoring of hydro-thermal activity. J. Geophys. Res. 115, B03205. https://doi.org/10.1029/2008JB006258 (2010).
5. Hurwitz, S. & Lowenstern, J. B. Dynamics of the Yellowstone hydrothermal system. Rev. Geophys. 52, 375–411. https://doi.org/10.1002/2014RG000452 (2014).
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