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TitleSource model for the Copahue volcano magma plumbing system constrained by InSAR surface deformation observations
AuthorLundgren, P; Nikkhoo, M; Samsonov, S V; Milillo, P; Gil-Cruz, F; Lazo, J
SourceJournal of Geophysical Research, Solid Earth vol. 122, 2017 p. 5729-5747, https://doi.org/10.1002/2017JB014368 (Open Access)
Year2017
Alt SeriesNatural Resources Canada, Contribution Series 20170205
PublisherWiley-Blackwell
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
AreaAgrio-Caviahue; Chile; Argentina
Lat/Long WENS -71.3333 -70.9167 -37.7500 -38.0000
Subjectsremote sensing; volcanoes; deformation; radar imagery; seismicity; faults, normal; faults, strike-slip; modelling; RADARSAT-2; COSMO-SkyMed; volcanic eruptions; caldera
Illustrationslocation maps; satellite images; plots; graphs; tables
Released2017 07 20
AbstractCopahue volcano straddling the edge of the Agrio-Caviahue caldera along the Chile-Argentina border in the southern Andes has been in unrest since inflation began in late 2011. We constrain Copahue's source models with satellite and airborne interferometric synthetic aperture radar (InSAR) deformation observations. InSAR time series from descending track RADARSAT-2 and COSMO-SkyMed data span the entire inflation period from 2011 to 2016, with their initially high rates of 12 and 15 cm/yr, respectively, slowing only slightly despite ongoing small eruptions through 2016. InSAR ascending and descending track time series for the 2013 - 2016 time period constrain a two-source compound dislocation model, with a rate of volume increase of 13 × 106 m3/yr. They consist of a shallow, near-vertical, elongated source centered at 2.5 km beneath the summit and a deeper, shallowly plunging source centered at 7 km depth connecting the
shallow source to the deeper caldera. The deeper source is located directly beneath the volcano tectonic seismicity with the lower bounds of the seismicity parallel to the plunge of the deep source. InSAR time series also show normal fault offsets on the NE flank Copahue faults. Coulomb stress change calculations for right-lateral strike slip (RLSS), thrust, and normal receiver faults show positive values in the north caldera for both RLSS and normal faults, suggesting that northward trending seismicity and Copahue fault motion within
the caldera are caused by the modeled sources. Together, the InSAR-constrained source model and the seismicity suggest a deep conduit or transfer zone where magma moves from the central caldera to Copahue's upper edifice.
GEOSCAN ID305975