Geodetic GNSS observations at 43 sites well distributed over the Southern Patagonian Icefield region yield site velocities with a mean accuracy of 1 mm/a and 6 mm/a for the horizontal and vertical components, respectively. These velocities are analyzed to reveal the magnitudes and patterns of vertical and horizontal present-day crustal deformation as well as their primary driving processes. The observed vertical velocities confirm a rapid uplift, with rates peaking at 41 mm/a, causally related to glacial-isostatic adjustment (GIA). They yield now an unambiguous preference between two competing GIA models. Remaining discrepancies between the preferred model and our observations point toward an effective upper mantle viscosity even lower than...
We present crustal velocities for 29 continuously recording GPS stations from the southern central A...
[1] A new Global Positioning System (GPS)-derived velocity field for the Andes mountains (26°-36°S) ...
The subduction of the Nazca oceanic plate under the South American plate in the south-central Andes ...
Thirty‒one GPS geodetic measurements of crustal uplift in southernmost South America determined extr...
Vertical site velocities determined by geodetic GPS observations in the Lago Fagnano area, Tierra de...
The geographic coincidence of the Chile Ridge slab window and the Patagonia ice fields offers a uniq...
The two main causes of global-scale secular deformation of the Earth are tectonic plate motion and G...
The present-day deformation of the earth crust in the Argentine part of Tierra del Fuego main island...
The aim of this research was to analyse the deformation in an intraplate region of southeastern Sout...
Surface mass transfer produces changes in the terrestrial geometric reference frame that are clearly...
In this study we present the contemporary crustal deformation field along the central and southern A...
Glacial isostatic adjustment (GIA) is the main cause of deformation in intraplate North America. Her...
In this work we have analyzed the results of temporal geodetic variations associated with tectonic d...
Across the extreme south of Patagonia, the Magallanes-Fagnano Fault (MFF) accommodates the left-late...
Global Positioning System (GPS) measurements provide the first direct measurement of plate motion an...
We present crustal velocities for 29 continuously recording GPS stations from the southern central A...
[1] A new Global Positioning System (GPS)-derived velocity field for the Andes mountains (26°-36°S) ...
The subduction of the Nazca oceanic plate under the South American plate in the south-central Andes ...
Thirty‒one GPS geodetic measurements of crustal uplift in southernmost South America determined extr...
Vertical site velocities determined by geodetic GPS observations in the Lago Fagnano area, Tierra de...
The geographic coincidence of the Chile Ridge slab window and the Patagonia ice fields offers a uniq...
The two main causes of global-scale secular deformation of the Earth are tectonic plate motion and G...
The present-day deformation of the earth crust in the Argentine part of Tierra del Fuego main island...
The aim of this research was to analyse the deformation in an intraplate region of southeastern Sout...
Surface mass transfer produces changes in the terrestrial geometric reference frame that are clearly...
In this study we present the contemporary crustal deformation field along the central and southern A...
Glacial isostatic adjustment (GIA) is the main cause of deformation in intraplate North America. Her...
In this work we have analyzed the results of temporal geodetic variations associated with tectonic d...
Across the extreme south of Patagonia, the Magallanes-Fagnano Fault (MFF) accommodates the left-late...
Global Positioning System (GPS) measurements provide the first direct measurement of plate motion an...
We present crustal velocities for 29 continuously recording GPS stations from the southern central A...
[1] A new Global Positioning System (GPS)-derived velocity field for the Andes mountains (26°-36°S) ...
The subduction of the Nazca oceanic plate under the South American plate in the south-central Andes ...