Color poster with maps, diagrams, photographs, and graphs.The south-central Andes are characterized by latitudinal stratigraphic variations that reflect changes in the rate and pattern of orogenic exhumation. Detailed analyses, including conglomerate clast counts, detrital zircon studies, and zircon Hf isotopic analyses, constrain the timing and pattern of an eastward propagating fold and thrust system that has influenced Andean deformation since early Miocene time. The primary objective of this study was to assess the influence of variations in subduction geometry along the Andean margin on basin development and evolution.University of Wisconsin--Eau Claire Office of Research and Sponsored Programs
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
Evolution of the Subandean fold-thrust belt and adjacent Chaco foreland basin since their inception ...
The Catan Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
The Andes Mountains provide an ideal natural laboratory to analyze the relationship between the tect...
In this work we study the evolution of one particular segment of the Southern Central Andes, the nor...
Artículo de publicación ISIThe southern Patagonian Andes constitute the narrow, high-latitude end of...
The Andean Cordilleran orogenic system stretches over 7,000 km along the western margin of South Ame...
AbstractThe temporal transition from backarc extension to retroarc shortening is a fundamental proce...
The Alto Tunuyán Foreland Basin in western Argentina is located immediately south of the flat-slab s...
The intraplate fault-block mountains and intermontane deposits of the Gastre Basin, which are record...
The Pampas plain (30°–41°S) has historically been considered as a sector that evolved independently ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
The stratigraphic and sedimentological characteristics of the Payogastilla Group represent important...
Despite their geodynamic significance, the stratigraphy and paleoenvironments of the lower-middle Mi...
Retroarc foreland basins in contractional arc settings contain evidence of temporal and spatial vari...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
Evolution of the Subandean fold-thrust belt and adjacent Chaco foreland basin since their inception ...
The Catan Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
The Andes Mountains provide an ideal natural laboratory to analyze the relationship between the tect...
In this work we study the evolution of one particular segment of the Southern Central Andes, the nor...
Artículo de publicación ISIThe southern Patagonian Andes constitute the narrow, high-latitude end of...
The Andean Cordilleran orogenic system stretches over 7,000 km along the western margin of South Ame...
AbstractThe temporal transition from backarc extension to retroarc shortening is a fundamental proce...
The Alto Tunuyán Foreland Basin in western Argentina is located immediately south of the flat-slab s...
The intraplate fault-block mountains and intermontane deposits of the Gastre Basin, which are record...
The Pampas plain (30°–41°S) has historically been considered as a sector that evolved independently ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
The stratigraphic and sedimentological characteristics of the Payogastilla Group represent important...
Despite their geodynamic significance, the stratigraphy and paleoenvironments of the lower-middle Mi...
Retroarc foreland basins in contractional arc settings contain evidence of temporal and spatial vari...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
Evolution of the Subandean fold-thrust belt and adjacent Chaco foreland basin since their inception ...
The Catan Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...