Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94850/1/tect1973.pd
The Abancay deflection (12-13.5°S), forming the northern edge of the Altiplano in the Central Andes ...
The southern Puna Plateau of the central Andes offers an excellent opportunity to (1) advance our un...
Within the Central Andes of NW Argentina, the spatiotemporal distribution and style of deformation i...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95425/1/tect1910.pd
none11siIn this paper, we merge more than 200 new apatite and zircon (U-Th)/He analyses and 21 apati...
analysis reveal rapid cooling during middle Eocene– late Oligocene and late Miocene–Pliocene exhumat...
The Andes are an ideal setting to explore orogenic wedge evolution and the cyclical tectonic process...
The Central Andes between 18°S and 36°S latitude strike north-south for 2000 km along the Chilean su...
The Andean Plateau of north‐western Argentina (Puna) at a mean elevation of ca. 4.2 km constitutes t...
The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Fro...
The Andean belt in South America is a first-order topographic feature on Earth. Significant differen...
The Abancay Deflection, forming the northern edge of the Altiplano in the Peruvian Andes, is a remar...
Spatiotemporal patterns of deformation and exhumation in the central Andes are key parameters for re...
The Andes of South America display the classic plate tectonic setting of oceanic-continental converg...
To better constrain the orogenic growth of the Andean chain, we investigated the time-Temperature pa...
The Abancay deflection (12-13.5°S), forming the northern edge of the Altiplano in the Central Andes ...
The southern Puna Plateau of the central Andes offers an excellent opportunity to (1) advance our un...
Within the Central Andes of NW Argentina, the spatiotemporal distribution and style of deformation i...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95425/1/tect1910.pd
none11siIn this paper, we merge more than 200 new apatite and zircon (U-Th)/He analyses and 21 apati...
analysis reveal rapid cooling during middle Eocene– late Oligocene and late Miocene–Pliocene exhumat...
The Andes are an ideal setting to explore orogenic wedge evolution and the cyclical tectonic process...
The Central Andes between 18°S and 36°S latitude strike north-south for 2000 km along the Chilean su...
The Andean Plateau of north‐western Argentina (Puna) at a mean elevation of ca. 4.2 km constitutes t...
The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Fro...
The Andean belt in South America is a first-order topographic feature on Earth. Significant differen...
The Abancay Deflection, forming the northern edge of the Altiplano in the Peruvian Andes, is a remar...
Spatiotemporal patterns of deformation and exhumation in the central Andes are key parameters for re...
The Andes of South America display the classic plate tectonic setting of oceanic-continental converg...
To better constrain the orogenic growth of the Andean chain, we investigated the time-Temperature pa...
The Abancay deflection (12-13.5°S), forming the northern edge of the Altiplano in the Central Andes ...
The southern Puna Plateau of the central Andes offers an excellent opportunity to (1) advance our un...
Within the Central Andes of NW Argentina, the spatiotemporal distribution and style of deformation i...