• Aucun résultat trouvé

Combining InSAR and GNSS to Track Magma Transport at Basaltic Volcanoes

N/A
N/A
Protected

Academic year: 2021

Partager "Combining InSAR and GNSS to Track Magma Transport at Basaltic Volcanoes"

Copied!
27
0
0

Texte intégral

Loading

Figure

Figure 1. Piton de la Fournaise (PdF) setting. (A) Location of Reunion Island; (B) Shaded topography of PdF volcano and location of the GNSS monitoring network
Figure 2. (Top) Temporal evolution of baseline changes recorded between two pairs of permanent GNSS stations (SNEG and DSRG and BORG and DERG; see Figure 1 for station locations) between 29 February
Figure 3. Wrapped interferograms used in this study. (Left column) Data acquired on ascending orbits;
Figure 4. Use of the different data sets in our modeling strategy.
+7

Références

Documents relatifs

New petrological data on eruption products and experimental results are integrated and a model for the evolution of the La Soufrière (Guadeloupe, Lesser Antilles

The effects of root thickness, soil type and the water content of the surrounding soil on the contrast between soil and roots in NR images has not been quantified and the capability

Multiplication Avec Les Chiffres Romains (A) Réponses.. Répondez à chaque question en

If the reservoir is at a critical equilibrium and connected to the summit lava lake, as indicated by the petrographical data [Demant et al., 1994], this stress change might

Following ten days of explosive activity, which included pyroclastic flows and falls, chemically identical lava began effusing from the same vents as continuing pyroclastic

Contours are at 100 m intervals (a) The volcano after collapse of the Skaros caldera, which happened some time before the first Skaros lava was erupted at 69 ± 7 ka (b) The

A number of distributed network protocols for reliable data transmission, connectivity test, shortest path and topology broadcast have been proposed with claims that

Eventually, we evaluate the applicability of monitoring flow conditions from observed ground deformation by using simplified conduit flow models, coupled with elastic deformation in