Low-pressure-high-temperature metamorphism during extension in a Jurassic magmatic arc, Central Pontides, Turkey

Keyphrases

• Turkey 100%
• Eastern Pontides 100%
• Low Pressure 100%
• Magmatic Arc 100%
• Metamorphic Rocks 100%
• High-temperature Metamorphism 100%
• Biotite 66%
• Pontides 66%
• Metamorphism 66%
• Crustal Melting 66%
• Ultrahigh-temperature Metamorphism 66%
• Plagioclase 33%
• Iran 33%
• Silica 33%
• High Temperature 33%
• Mineral Assemblage 33%
• Middle Jurassic 33%
• Volcanic Rocks 33%
• K-feldspar 33%
• Eurasia 33%
• Heat Flow 33%
• Shallow Levels 33%
• Migmatite 33%
• Gneiss 33%
• Zircon U-Pb 33%
• Magmatism 33%
• Granitoids 33%
• Mantle Melting 33%
• Garnet 33%
• Cordierite 33%
• Ultramafic 33%
• Caucasus 33%
• Northern Turkey 33%
• Metamorphic Belt 33%
• Active Margin 33%
• Metamorphic Conditions 33%
• Mineral Equilibria 33%
• Magmatic Rocks 33%
• Continental Magmatic Arc 33%
• Crimea 33%
• Peak Metamorphism 33%
• Ar-Ar Age 33%
• Extensional Tectonic Environment 33%
• Dioritic Enclaves 33%
• Inherited Zircon 33%
• High Heat Flow 33%
• Marine Basin 33%
• Jurassic Granitoids 33%
• Contractional Deformation 33%
• Arc Signature 33%

Earth and Planetary Sciences

• High Temperature Metamorphism 100%
• Metamorphic Rock 100%
• Peridotite 66%
• Zircon 66%
• Granitoid 66%
• Magmatism 33%
• Volcanic Rock 33%
• Middle Jurassic 33%
• Gneiss 33%
• Migmatite 33%
• Extensional Tectonics 33%
• Active Margin 33%
• Garnet 33%
• Volcaniclastic 33%
• Cordierite 33%