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The August 2019 Piton de la Fournaise (La Reunion Island) Eruption: Analysis of the Multi-Source Deformation Pattern Detected through Sentinel-1 DInSAR Measurements
被引:3
|作者:
Valerio, Emanuela
[1
]
De Luca, Claudio
[1
]
Lanari, Riccardo
[1
]
Manzo, Mariarosaria
[1
]
Battaglia, Maurizio
[2
]
机构:
[1] CNR, IREA, I-80124 Naples, Italy
[2] Sapienza Univ Roma, Dipartimento Sci Terra, I-00185 Rome, Italy
基金:
欧盟地平线“2020”;
关键词:
Piton de la Fournaise;
eruptions modeling;
volcano deformation;
Sentinel-1 DInSAR measurements;
analytical modeling;
multi-source deformation;
APRIL;
2007;
ERUPTION;
SURFACE DEFORMATION;
INDIAN-OCEAN;
LARGE AREAS;
VOLCANO;
EARTHQUAKES;
PROPAGATION;
COLLAPSE;
DISPLACEMENT;
EVOLUTION;
D O I:
10.3390/rs14071762
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
Piton de la Fournaise is one of the most active worldwide volcanoes, located on the southeastern part of La Reunion Island. In this work, we focus on the eruption that occurred on the southeastern flank of this volcano, inside the Enclos Fouque caldera, from 11 to 15 August 2019. This distal event was characterized by the opening of two eruptive fissures and accompanied by shallow volcano-tectonic earthquakes. We exploit the ground displacements using Sentinel-1 Differential Interferometric Synthetic Aperture Radar (DInSAR) measurements, which include the ground deformations generated during both the pre- and co-eruptive phases. To investigate the sources responsible for the detected ground displacements, we perform an analytical modeling of the retrieved DInSAR measurements. Our results reveal the presence of five volcanic sources (i.e., one sill-like source and four dikes), whose concomitant action during the pre- and co-eruptive phases generated the complex detected deformation pattern. The retrieved volcanic sources correlate well with the location of the opened fissures, the spatial distribution and the temporal evolution of the recorded seismicity, and other geophysical evidence already known in the literature.
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页数:14
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