Crustal-scale structural architecture in central Chile based on seismicity and surface geology: Implications for Andean mountain building

Keyphrases

• Cordillera 100%
• Central Chile 100%
• Subduction Zone 100%
• Andean Mountains 100%
• Mountain Building 100%
• Structural Architecture 100%
• Seismicity 100%
• Surface Geology 100%
• Tectonics 50%
• Andes 50%
• Crustal Thickening 50%
• Blueschist 50%
• Subducting Slab 50%
• Chilean Margin 50%
• Andean Orogeny 50%
• Plate Convergence 50%
• Plate Interface 50%
• Andean Subduction 50%
• Subduction Processes 50%
• Andean Orogenesis 50%
• Upper Mantle 50%
• Ramp-flat 50%
• Detachment Structure 50%
• Rheology Control 50%
• Simple Shear Deformation 50%
• Contact Mark 50%
• Flat Structure 50%
• Seismogenic 50%
• Eclogite 50%
• Yield Envelope 50%
• Deformation Mode 50%
• First-order Features 50%

Earth and Planetary Sciences

• Chile 100%
• Subduction Zone 100%
• Geology 100%
• Mountain Building 100%
• Seismicity 100%
• Tectonics 50%
• Orogeny 50%
• Andes 50%
• Crustal Thickening 50%
• Blueschist 50%
• Andean Orogeny 50%
• Plate Convergence 50%
• Yield Strength 50%
• Eclogite 50%
• Upper Mantle 50%