Dome permeability and fluid circulation at La Soufrière de Guadeloupe implied from soil CO$$_2$$ degassing, thermal flux and self-potential
Author:
Funder
Institut national des sciences de l’Univers
Université Clermont-Auvergne
Institut de Physique du Globe de Paris
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00445-024-01713-z.pdf
Reference99 articles.
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2. Aizawa K (2008) Classification of self-potential anomalies on volcanoes and possible interpretations for their subsurface structure. J Volcanol Geoth Res 175:253–268. https://doi.org/10.1016/j.jvolgeores.2008.03.011
3. Aizawa K, Ogawa Y, Ishido T (2009) Groundwater flow and hydrothermal systems within volcanic edifices: Delineation by electric self-potential and magnetotellurics. J Geophys Res, Solid Earth 114(1). https://doi.org/10.1029/2008JB005910
4. Allard P, Aiuppa A, Beauducel F et al (2014) Steam and gas emission rate from La Soufrière volcano, Guadeloupe (Lesser Antilles): Implications for the magmatic supply during degassing unrest. Chem Geol 384:76–93. https://doi.org/10.1016/j.chemgeo.2014.06.019
5. Aubert M (1999) Practical evaluation of steady heat discharge from dormant active volcanoes: case study of Vulcarolo fissure (Mount Etna, Italy). J Volcanol Geoth Res 92(3–4):413–429. https://doi.org/10.1016/S0377-0273(99)00088-8
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