The relationship between long-lived deep crustal lineaments and the locations of magmatic
centers and associated mineral deposits has been investigated in the Puna region of …

Late Cenozoic Andean deformation in the Pampean segment of Argentina and Chile (27°
00′–33° 30′ S) provides an exceptional opportunity to study the orogenic effects of flat …

We quantitatively analyse the spatial pattern of deformation partitioning and of temporal
accumulation of deformation in the Central Andes (15–26° S) with the aim of identifying …

The Andes, in particular their central parts, have been known as a preeminent Cu province
for more than 100 years and have been the source of many innovative metallogenic …

Low internal relief, aridity, and internal drainage characterize the Puna‐Altiplano Plateau
and the Tibetan Plateau and the Tarim basin. Structurally, these areas are reverse fault …

Topographically, the Puna plateau of northwestern Argentina is the southern continuation of
the Bolivian Altiplano. Its thickening and consecutive uplift result from the Andean orogeny …

Intraplate compressional features, such as inverted extensional basins, upthrust basement
blocks and whole lithospheric folds, play an important role in the structural framework of …

Using available information on the magnitude and age of tectonic shortening, as well as
paleomagnetically determined tectonic rotations, we have run a series of 2‐D map view …

Since its release in June 2005, Google Earth has been bringing satellite images of our
planet into our homes, or at least to those homes with broadband connections. Computer …

The southernmost Andes form an orocline, between the Patagonian cordillera, trending N–
S, and the Fueguian cordilleras, trending E–W. On the foreland side is the Magellan Basin …