Diverse techniques have been applied over the past decade to quantify the uplift history of
the central Andean Plateau (AP). In this study, opposing models for surface uplift are …

Con la ayuda de un análisis flexural de la correlación entre relieve y gravedad, se investiga
qué factores controlan la segmentación del sistema de convergencia andino entre los 15 y …

We present a new set of contour maps of the seismic structure of South America and the
surrounding ocean basins. These maps include new data, hel** to constrain crustal …

The largest accumulations of rhyolitic melt in the upper crust occur in voluminous silicic
crystal mushes, which sometimes erupt as unzoned, crystal-rich ignimbrites, but are most …

The Andean volcanic arc includes over 200 potentially active Quaternary volcanoes, and at
least 12 giant caldera/ignimbrite systems, occurring in four separate segments referred to as …

We forward modeled the Bouguer anomaly in a region encompassing the Pacific Ocean
(85° W) and the Andean margin (60° W) between northern Peru (5° S) and Patagonia (45° …

P-to-S converted waves at the continental Moho together with waves multiply reflected
between the Earth's surface and the Moho have been used to estimate the Moho depth and …

Integrated studies and revisions of sedimentary basins and associated magmatism in Peru
and Bolivia (8–22° S) show that this part of western Gondwana underwent rifting during the …

Understanding Neogene arc crustal thickening in the central Andes requires (1) some
estimate of initial pre‐Neogene (prior to 26 Ma) crustal thicknesses and (2) mechanisms that …

A long‐period magnetotelluric study was carried out in the central Andes between latitudes
19.5° S and 21° S along two almost parallel profiles of 220 and 380 km length, respectively …