Tectonic evolution of NW Iberia during the Paleozoic inferred from the geochemical record of detrital rocks in the Cantabrian Zone

Keyphrases

• Tectonic Evolution 100%
• Geochemical Data 100%
• Ediacaran 100%
• NW Iberia 100%
• Cantabrian Zone 100%
• Sedimentary Sequence 66%
• Early Permian 66%
• Passive Margin 66%
• Gondwana 66%
• Oroclinal Buckling 66%
• Tectonics 33%
• Tectonic Setting 33%
• Late Permian 33%
• Late Carboniferous 33%
• Iberia 33%
• Age Distribution 33%
• Variscan Orogeny 33%
• Permian Age 33%
• Sm-Nd 33%
• Active Continental Margin 33%
• Detrital Zircon Ages 33%
• Zircon Age 33%
• Ribbon Continent 33%
• Sm-Nd Isotopes 33%
• Laurussia 33%
• Active Margin 33%
• Lithospheric Foundering 33%
• Illite Crystallinity 33%
• Ordovician 33%
• Northern Gondwana Margin 33%
• Late Devonian 33%
• Far-field Effect 33%

Earth and Planetary Sciences

• Tectonic Evolution 100%
• Permian 100%
• Gondwana 100%
• Ediacaran 100%
• Sedimentary Sequence 66%
• Zircon 66%
• Passive Margin 66%
• Continental Shelf 33%
• Geochemistry 33%
• Tectonics 33%
• Hercynian Orogeny 33%
• Tectonic Setting 33%
• Continent 33%
• Crystallinity 33%
• Ordovician 33%
• Active Margin 33%
• Late Devonian 33%
• Illite 33%
• Age Distribution 33%