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Unconformity development in retroarc foreland basins: implications for the geodynamics of Andean-type margins
Unconformities in foreland basins may be generated by tectonic processes that operate in
the basin, the adjacent fold–thrust belt or the broader convergent margin. Foreland basin …
the basin, the adjacent fold–thrust belt or the broader convergent margin. Foreland basin …
Oligocene to present shallow subduction beneath the southern Puna plateau
The southern Puna plateau is a conspicuous example of a high-elevation orogenic plateau
in a non-collisional setting. This orogenic sector is currently located above an anomalously …
in a non-collisional setting. This orogenic sector is currently located above an anomalously …
Southward expanding plate coupling due to variation in sediment subduction as a cause of Andean growth
Growth of the Andes has been attributed to Cenozoic subduction. Although climatic and
tectonic processes have been proposed to be first-order mechanisms, their interaction and …
tectonic processes have been proposed to be first-order mechanisms, their interaction and …
Reviewing the geodynamic impact of aseismic ridges subduction on the tectonic-magmatic evolution of the Southern Puna plateau
W Báez, E Bustos, A Chiodi, HPA García… - Journal of South …, 2023 - Elsevier
Abstract The Southern Puna (∼ 24° S to 27° S) is an outstanding segment of the Central
Andes where the subduction of aseismic ridges, multi-scale lithospheric foundering, and the …
Andes where the subduction of aseismic ridges, multi-scale lithospheric foundering, and the …
Kinematic Evolution of the Santa Bárbara System in the Foreland of the Central Andes of Northwestern Argentina (26° S)
Compared to the thin‐skinned Subandean foreland fold‐and‐thrust belt of northern
Argentina and Bolivia, the tectonically active morphotectonic province of the Santa Bárbara …
Argentina and Bolivia, the tectonically active morphotectonic province of the Santa Bárbara …
Tectonic and climatic significance of Oligocene-Miocene eolian sandstones in the Andean foreland basin of Argentina
Abstract Late Oligocene-early Miocene aridification in the retroarc foreland basin adjacent to
the southern central Andes was recorded by widespread eolian conditions that coincided …
the southern central Andes was recorded by widespread eolian conditions that coincided …
Development of an incipient Paleogene topography between the present‐day Eastern Andean Plateau (Puna) and the Eastern Cordillera, southern Central Andes …
The structural and topographic evolution of orogenic plateaus is an important research topic
because of its impact on atmospheric circulation patterns, the amount and distribution of …
because of its impact on atmospheric circulation patterns, the amount and distribution of …
Eocene to Quaternary deformation of the Southern Puna Plateau: Thermochronology, geochronology, and structural geology of an Andean hinterland basin (NW …
Cordilleran orogens are complex tectonic systems, strongly influenced by lithospheric
deformation and exhumation. However, in the type region of the Central Andes, the timing …
deformation and exhumation. However, in the type region of the Central Andes, the timing …
Stratigraphic response to fragmentation of the Miocene Andean foreland basin, NW Argentina
Foreland basins are sensitive recorders of spatiotemporal variations in tectonic and climatic
forcing associated with an approaching orogenic front. Thus, analysis of foreland deposits …
forcing associated with an approaching orogenic front. Thus, analysis of foreland deposits …
Tectonic control on drainage evolution in broken forelands: Examples from NW Argentina
Planform drainage patterns in orogens reflect the initial control of local structures, resulting
in strike‐parallel longitudinal drainage, and the subsequent influence of regional slopes that …
in strike‐parallel longitudinal drainage, and the subsequent influence of regional slopes that …