Alpine Ductile Deformation of the Upper Iberian Collided Margin (Eaux-Chaudes Massif, West-Central Pyrenean Hinterland, France)

Keyphrases

• France 100%
• Massif 100%
• Ductile Deformation 100%
• Pyrenees 50%
• Upper Cretaceous 50%
• Carbonate Rocks 50%
• Thrust Sheets 50%
• Shale 50%
• Keuper 50%
• Fold Nappe 50%
• Carbonate 25%
• Foliation 25%
• Tectonics 25%
• Structural Change 25%
• Autochthonous 25%
• Deformation Condition 25%
• Palaeozoic Basement 25%
• Cenozoic 25%
• Evaporites 25%
• Axial Zone 25%
• Structural Variation 25%
• Cross-section Construction 25%
• Alpine Orogeny 25%
• Geological Mapping 25%
• Meso-Cenozoic 25%
• Pluton 25%
• Paleozoic Rocks 25%
• Metasediments 25%
• Structural Style 25%
• Ductile Shearing 25%
• Kinematic Indicators 25%
• Stretching Lineation 25%
• Fold-and-thrust 25%
• Inlier 25%
• Rifted Margin 25%
• Upper Paleozoic 25%
• Ophites 25%
• Deep-seated Deformation 25%

Earth and Planetary Sciences

• Upper Cretaceous 100%
• Ductile Deformation 100%
• Keuper 100%
• Carbonate Rock 100%
• France 100%
• Devonian 50%
• Evaporite 50%
• Hercynian Orogeny 50%
• Alpine Orogeny 50%
• Geological Mapping 50%
• Silurian 50%
• Lineation 50%
• Structural Change 50%
• Metasediment 50%
• Inlier 50%
• Tectonics 50%