Andean orogenesis is expressed in the diverse deformational records of crustal structures and sedimentary basins in western South America. Here we summarize retroarc structural styles within the Andean orogenic belt and foreland basin system through consideration of regional contractional fault geometries, their kinematic interactions with other structures, and the comparative involvement of crystalline basement and sedimentary cover rocks. In assessing the controls on structural style, we emphasize the importance of precursor conditions and employ the concept of tectonic inheritance to identify four factors that influence Andean deformation. (1) Structural inheritance involves the reactivation of preexisting faults or basement fabrics and ...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
We present the first complete balanced cross-section of the Argentinean Andes at 35ºS. Based on an e...
The Malargüe fold-and-thrust belt is a thick-skinned belt developed in Miocene-Pliocene times during...
The Chos Malal fold and thrust belt is a thick-skinned mountain belt that deformed the Mesozoic de...
The Andean Orogeny in South America has lasted over 100 Ma. It comprises the Peruvian, Incaic and Qu...
The Andean Orogeny in South America has lasted over 100 Ma. It comprises the Peruvian, Incaic and Qu...
This chapter focuses on the structural styles of the Villa Unión-San Isidro basement-involved fold a...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
Structures mapped in the southern Cordillera Oriental of the Andes show an unexpected geometry in an...
Superposed structural fabrics in the easternmost Fuegian Andes reveal two distinct, non-coaxial defo...
Structures mapped in the southern Cordillera Oriental of the Andes show an unexpected geometry in an...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
In the southern Central Andes, the Andean foreland was deformed due to Neogene shallowing of the Naz...
Deformation and uplift in the Andes are a result of the subduction of the Nazca plate below South Am...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
We present the first complete balanced cross-section of the Argentinean Andes at 35ºS. Based on an e...
The Malargüe fold-and-thrust belt is a thick-skinned belt developed in Miocene-Pliocene times during...
The Chos Malal fold and thrust belt is a thick-skinned mountain belt that deformed the Mesozoic de...
The Andean Orogeny in South America has lasted over 100 Ma. It comprises the Peruvian, Incaic and Qu...
The Andean Orogeny in South America has lasted over 100 Ma. It comprises the Peruvian, Incaic and Qu...
This chapter focuses on the structural styles of the Villa Unión-San Isidro basement-involved fold a...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
Structures mapped in the southern Cordillera Oriental of the Andes show an unexpected geometry in an...
Superposed structural fabrics in the easternmost Fuegian Andes reveal two distinct, non-coaxial defo...
Structures mapped in the southern Cordillera Oriental of the Andes show an unexpected geometry in an...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
In the southern Central Andes, the Andean foreland was deformed due to Neogene shallowing of the Naz...
Deformation and uplift in the Andes are a result of the subduction of the Nazca plate below South Am...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, general...
We present the first complete balanced cross-section of the Argentinean Andes at 35ºS. Based on an e...
The Malargüe fold-and-thrust belt is a thick-skinned belt developed in Miocene-Pliocene times during...