Complex paths of magma propagation at Fernandina (Galápagos): The coexistence of circumferential and radial dike intrusion during the January 2020 eruption
Author:
Funder
Earth Sciences Division
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
https://link.springer.com/content/pdf/10.1007/s00445-023-01688-3.pdf
Reference52 articles.
1. Acocella V, Neri M (2003) What makes flank eruptions? The 2001 Etna eruption and its possible triggering mechanisms. Bull Volcanol 65:517–529. https://doi.org/10.1007/s00445-003-0280-3
2. Acocella V, Di Lorenzo R, Newhall C, Scandone R (2015) An overview of recent (1988 to 2014) caldera unrest: Knowledge and perspectives. Rev Geophys 53:896–955. https://doi.org/10.1002/2015RG000492
3. Bagnardi M, Amelung F (2012) Space‐geodetic evidence for multiple magma reservoirs and subvolcanic lateral intrusions at Fernandina Volcano, Galápagos Islands. J Geophys Res: Solid Earth 117 https://doi.org/10.1029/2012JB009465
4. Bagnardi M, Hooper A (2018) Inversion of surface deformation data for rapid estimates of source parameters and uncertainties: A Bayesian approach. Geochem Geophys Geosyst 19 https://doi.org/10.1029/2018GC007585
5. Bagnardi M, Amelung F, Poland MP (2013) A new model for the growth of basaltic shields based on deformation of Fernandina volcano, Galápagos Islands. Earth Planet Sci Lett 377:358–366. https://doi.org/10.1016/j.epsl.2013.07.016
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