RENEWED POST-ERUPTIVE UPLIFT FOLLOWING THE 2011-2012 RHYOLITIC ERUPTION OF CORDON CAULLE (SOUTHERN ANDES, CHILE): EVIDENCE FOR TRANSIENT EPISODES OF MAGMA RESERVOIR RECHARGE DURING 2012-2018

Francisco Delgado; Matthew Pritchard; Sergey Samsonov; Loreto Cordova

doi:10.5281/zenodo.1292329

Published June 18, 2018 | Version v1

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RENEWED POST-ERUPTIVE UPLIFT FOLLOWING THE 2011-2012 RHYOLITIC ERUPTION OF CORDON CAULLE (SOUTHERN ANDES, CHILE): EVIDENCE FOR TRANSIENT EPISODES OF MAGMA RESERVOIR RECHARGE DURING 2012-2018

1. Cornell University
2. Canada Centre for Mapping and Earth Observation, Natural Resources Canada
3. OVDAS, Sernageomin

InSAR CSK descending time series for the point of maximum ground deformation (-72.210556, -40.491389). This is the time series used in Figure 8 of the manuscript.

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Created: June 18, 2018
Modified: January 20, 2020

RENEWED POST-ERUPTIVE UPLIFT FOLLOWING THE 2011-2012 RHYOLITIC ERUPTION OF CORDON CAULLE (SOUTHERN ANDES, CHILE): EVIDENCE FOR TRANSIENT EPISODES OF MAGMA RESERVOIR RECHARGE DURING 2012-2018

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