Shallow magma convection evidenced by excess degassing and thermal radiation during the dome-forming Sabancaya eruption (2012–2020)

International audience ; We used a large set of satellite-(visible, infrared, and radar images from Planetscope, MODIS, VIIRS, Sentinel2, Landsat 8, and Sentinel 1) and ground-based data (optical images, SO 2 flux, shallow seismicity) to describe and characterize the activity of the Sabancaya volcano during the unrest and eruption phases that occurred between 2012 and 2020. The unrest phase (2012-2016) was characterized by increasing gas and thermal flux, sourced by a convective magma column rising along with the remnants of a buried plug still permeable to fluid flow. Conversely, a new condui... Mehr ...

Verfasser: Coppola, Diego
Valade, S
Masias, P
Laiolo, M
Massimetti, F
Campus, A
Aguilar, R
Anccasi, R
Apaza, F
Ccallata, B
Cigolini, C
Cruz, L, F
Finizola, Anthony
Gonzales, K
Macedo, O
Miranda, R
Ortega, M
Paxi, R
Taipe, E
Valdivia, D
Dokumenttyp: Artikel
Erscheinungsdatum: 2022
Verlag/Hrsg.: HAL CCSD
Schlagwörter: Sabancaya / Dome-forming-eruption / Excess degassing / Excess radiation / Shallow magma convection / [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology / [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Sprache: Englisch
Permalink: https://search.fid-benelux.de/Record/base-26865201
Datenquelle: BASE; Originalkatalog
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Link(s) : https://hal.univ-reunion.fr/hal-03543369