The Evolution of the Chilean-Argentinean Andes

Chapter 1 Structure and Tectonics of the Chilean Convergent Margin from Wide-Angle Seismic Studies: A Review

Chapter 2 The Geometry of the Continental Wedge and Its Relation to the Rheology and Seismicity of the Chilean Interplate Boundary

Chapter 3 The Peru-Chile Margin from Global Gravity Field Derivatives

Chapter 4 Paleogeographic and Kinematic Constraints in the Tectonic Evolution of the Pre-Andean Basement Blocks

Chapter 5 The Pre-Andean Phases of Construction of the Southern Andes Basement in Neoproterozoic–Paleozoic Times

Chapter 6 The Famatinian Orogen Along the Protomargin of Western Gondwana: Evidence for a Nearly Continuous Ordovician Magmatic Arc Between Venezuela and Argentina

Chapter 7 The Early Stages of the Magmatic Arc in the Southern Central Andes

Chapter 8 A Provenance Analysis from the Lower Jurassic Units of the Neuquén Basin. Volcanic Arc or Intraplate Magmatic Input?

Chapter 9 The Jurassic Paleogeography of South America from Paleomagnetic Data

Chapter 10 Lower Jurassic to Early Paleogene Intraplate Contraction in Central Patagonia

Chapter 11 Mechanisms and Episodes of Deformation Along the Chilean–Pampean Flat-Slab Subduction Segment of the Central Andes in Northern Chile

Chapter 12 Cretaceous Orogeny and Marine Transgression in the Southern Central and Northern Patagonian Andes: Aftermath of a Large-Scale Flat-Subduction Event?

Chapter 13 Tectonic Rotations Along the Western Central Andes

Chapter 14 Paleogene Arc-Related Volcanism in the Southern Central Andes and North Patagonia (39°–41° S)

Chapter 15 Mantle Influence on Andean and Pre-Andean Topography

Chapter 16 Cenozoic Uplift and Exhumation of the Frontal Cordillera Between 30° and 35° S and the Influence of the Subduction Dynamics in the Flat Slab Subduction Context, South Central Andes

Chapter 17 The Structure of the Southern Central Andes (Chos Malal Fold and Thrust Belt)

Chapter 18 The Late Oligocene–Early Miocene Marine Transgression of Patagonia

Chapter 19 Neogene Growth of the Patagonian Andes

Chapter 20 The Late Paleogene to Neogene Volcanic Arc in the Southern Central Andes (28°–37° S)

Chapter 21 Basin Thermal Structure in the Chilean-Pampean Flat Subduction Zone