The deformation front of the Neuquén fold and thrust belt (~37°30′S) comprises kilometer-scale basement-involved anticlines, related to development of the Las Yeseras and Pampa Tril thrust systems, connected with awide frontal syncline. The interpretation of more than 70 seismic lines led to the construction of a time-structuremap at top of the Cuyo Group (Middle Jurassic), which shows a structural high east of the Tromen volcanoproduced by the superposition of thick-skinned structures. Moreover, data from 35 oil wells constrain the along-strike variations in structural reliefs. The structural relief of the Las Yeseras anticline increase from north tosouth, between ~1000 m and 2000 m, while the structural relief of the Pampa Tril anticline ...
The structure of basement-cored uplift mountains is fundamentally controlled by the geometry of the ...
This chapter is focused on the tectonic evolution of the North PatagonianAndes comprised between 38°...
The Agrio fold and thrust belt is an orogenic belt located in the Southern Central Andes (37°-38°S l...
The Chos Malal fold and thrust belt is a thick-skinned mountain belt that deformed the Mesozoic de...
The Chos Malal fold and thrust belt, formed during the Andean orogeny, is characterized by the invol...
Deformation and uplift in the Andes are a result of the subduction of the Nazca plate below South Am...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
This chapter focuses on the structural styles of the Villa Unión-San Isidro basement-involved fold a...
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland defor...
The Malargüe fold-and-thrust belt is a thick-skinned belt developed in Miocene-Pliocene times during...
In the southern Central Andes, the Andean foreland was deformed due to Neogene shallowing of the Naz...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
In the southern central Andes at 37–38°S latitude, the Chos Malal fold-and-thrust belt (FTB), which ...
The Neuquén Basin, developed in a retroarc setting in the central-west of Argentina, contains more t...
Curved traces are recurrent features of structural map-view patterns on different fold and thrust be...
The structure of basement-cored uplift mountains is fundamentally controlled by the geometry of the ...
This chapter is focused on the tectonic evolution of the North PatagonianAndes comprised between 38°...
The Agrio fold and thrust belt is an orogenic belt located in the Southern Central Andes (37°-38°S l...
The Chos Malal fold and thrust belt is a thick-skinned mountain belt that deformed the Mesozoic de...
The Chos Malal fold and thrust belt, formed during the Andean orogeny, is characterized by the invol...
Deformation and uplift in the Andes are a result of the subduction of the Nazca plate below South Am...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
This chapter focuses on the structural styles of the Villa Unión-San Isidro basement-involved fold a...
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland defor...
The Malargüe fold-and-thrust belt is a thick-skinned belt developed in Miocene-Pliocene times during...
In the southern Central Andes, the Andean foreland was deformed due to Neogene shallowing of the Naz...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
In the southern central Andes at 37–38°S latitude, the Chos Malal fold-and-thrust belt (FTB), which ...
The Neuquén Basin, developed in a retroarc setting in the central-west of Argentina, contains more t...
Curved traces are recurrent features of structural map-view patterns on different fold and thrust be...
The structure of basement-cored uplift mountains is fundamentally controlled by the geometry of the ...
This chapter is focused on the tectonic evolution of the North PatagonianAndes comprised between 38°...
The Agrio fold and thrust belt is an orogenic belt located in the Southern Central Andes (37°-38°S l...