An intrinsic feature of Cordillera-style orogenic systems is a spatial trend in the radiogenic
isotopic composition of subduction-related magmatism. Magmatism is most isotopically …

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

Abstract Two Early Paleozoic orogenic cycles in the Gondwana margin of NW Argentina
were driven by subduction, and interrupted by collision of continental ribbons of Laurentian …

We present stable hydrogen-isotope analyses of volcanic glass (δ Dg) and radiometric ages
(U–Pb zircon, U–Th calcite, AMS14C) from deformed sedimentary deposits in the vicinity of …

Abstract The Altiplano-Puna volcanic complex in the central Andes records a history of major
caldera-forming eruptions over the past 10 my Geophysical and geodetic data indicate that …

Magnetotelluric (MT) data were used to create a three-dimensional electrical resistivity
model of the Altiplano-Puna magma body (APMB) in the area surrounding Volcán Uturuncu …

The role of lithospheric architecture and the mantle in the genesis of iron oxide copper‐gold
(IOCG) deposits is controversial. Using the example of the Precambrian Gawler Craton …

A regional, balanced cross section is presented for the thin-skinned Tajik fold-and-thrust
belt, constrained by new structural and stratigraphic data, industrial well-log data, flexural …

The central Andes of Bolivia, northern Chile, and northwestern Argentina provide a unique
natural laboratory for understanding cordilleran mountain belts. Rapid convergence …

Abstract The Central Andes is a key global location to study the enigmatic relation between
volcanism and plutonism because it has been the site of large ignimbrite-forming eruptions …