|Measurement method(s):||InSAR, GPS - continuous, GPS - campaign|
|Duration of observation:||1995-2016 (InSAR), 2010-2016 (Continuous GPS) 2011-2016 (Campaign GPS)|
|Inferred cause of deformation:|||
|Characteristics of deformation:||
Uplift at the ‘Lazufre’ area, situated to the north of Cordon del Azufre and south of Lastarria volcano, was first detected in ERS interferograms from 1998 (Pritchard & Simons, 2002; Henderson & Pritchard, 2013). The rate of uplift accelerated between 1998 and 2005 up to a maximum rate of 3.5 cm / year and continued at this constant rate between 2005 and 2011 (Henderson and Pritchard, 2013).
|References:||'Pritchard, M. E., & Simons, M. (2002). A satellite geodetic survey of large-scale deformation of volcanic centres in the central Andes. Nature, 418(6894), 167-171. doi:10.1038/nature00872
\n', 'Henderson S. T., and M. E. Pritchard (2013), Decadal volcanic deformation in the Central Andes Volcanic Zone revealed by InSAR time series, Geochem. Geophys. Geosyst., 14, 1358–1374, doi:10.1002/ggge.20074.
\n', 'Scott T. Henderson, Francisco Delgado, Julie Elliott, Matthew E. Pritchard, Paul R. Lundgren (2017); Decelerating uplift at Lazufre volcanic center, Central Andes, from A.D. 2010 to 2016, and implications for geodetic models. Geosphere ; 13 (5): 1489–1505. doi: https://doi.org/10.1130/GES01441.1
\n', 'J. Ruch, T.R. Walter (2010), Relationship between the InSAR-measured uplift, the structural framework, and the present-day stress field at Lazufre volcanic area, central Andes.Tectonophysics, 492 (1–4), 133-140, https://doi.org/10.1016/j.tecto.2010.06.003.
\n', 'Pearse, J., and P. Lundgren (2013), Source model of deformation at Lazufre volcanic center, central Andes, constrained by InSAR time series, Geophys. Res. Lett., 40, 1059–1064, doi:10.1002/grl.50276.