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Deformation of the central Andean upper plate system—Facts, fiction, and constraints for plateau models
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 …
accumulation of deformation in the Central Andes (15–26° S) with the aim of identifying …
Style and history of Andean deformation, Puna plateau, northwestern Argentina
I Coutand, PR Cobbold, M de Urreiztieta, P Gautier… - …, 2001 - Wiley Online Library
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 …
the Bolivian Altiplano. Its thickening and consecutive uplift result from the Andean orogeny …
Paleogene building of the Bolivian Orocline: Tectonic restoration of the central Andes in 2‐D map view
C Arriagada, P Roperch, C Mpodozis, PR Cobbold - Tectonics, 2008 - Wiley Online Library
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 …
paleomagnetically determined tectonic rotations, we have run a series of 2‐D map view …
Distribution, timing, and causes of Andean deformation across South America
PR Cobbold, EA Rossello, P Roperch, C Arriagada… - 2007 - pubs.geoscienceworld.org
Abstract The Andean Orogeny in South America has lasted over 100 Ma. It comprises the
Peruvian, Incaic and Quechuan phases. The Nazca and South American plates have been …
Peruvian, Incaic and Quechuan phases. The Nazca and South American plates have been …
Counterclockwise rotation of late Eocene–Oligocene fore‐arc deposits in southern Peru and its significance for oroclinal bending in the central Andes
The results of a paleomagnetic study along the fore arc of southern Peru (15–18° S) and
northern Chile (18–19° S) are reported from middle to late Miocene ignimbrites (7 sites), late …
northern Chile (18–19° S) are reported from middle to late Miocene ignimbrites (7 sites), late …
[كتاب][B] The Andes: active subduction orogeny
Convergent plate margins and subduction zones are first order features sha** the Earth.
Convergent continental margins combine the majority of processes that affect the internal …
Convergent continental margins combine the majority of processes that affect the internal …
Growth of the Central Andean Plateau by tectonic segmentation is controlled by the gradient in crustal shortening
Crustal deformation, orocline formation, and growth of the central Andean plateau as well as
the mutual relations of these processes with climate are a matter of international debate …
the mutual relations of these processes with climate are a matter of international debate …
Structure and Cenozoic kinematics of the Eastern Cordillera, southern Bolivia (21 S)
The Eastern Cordillera is a main morphotectonic unit of the central Andes. In southern
Bolivia it is predominantly composed of Ordovician sedimentary rocks as thick as 10 km …
Bolivia it is predominantly composed of Ordovician sedimentary rocks as thick as 10 km …
Bending the Bolivian orocline in real time
RW Allmendinger, R Smalley Jr, M Bevis… - …, 2005 - pubs.geoscienceworld.org
Global positioning system (GPS) data from the central Andes record vertical axis rotations
that are consistently counterclockwise in Peru and Bolivia north of the bend in the mountain …
that are consistently counterclockwise in Peru and Bolivia north of the bend in the mountain …
Tectonics, climate, and landscape evolution of the southern central Andes: the Argentine Puna Plateau and adjacent regions between 22 and 30 S
RN Alonso, B Bookhagen, B Carrapa, I Coutand… - The Andes: active …, 2006 - Springer
The history of the Puna Plateau and its marginal basins and ranges in the Eastern Cordillera
and the northern Sierras Pampeanas structural provinces in northwestern Argentina …
and the northern Sierras Pampeanas structural provinces in northwestern Argentina …