Some remarks on the nature of mantle metasomatism beneath western Anatolian–Aegean region: Contrasting isotopic signatures recorded in the Miocene lavas from the Söke Basin

Keyphrases

• Lava 100%
• Isotopic Signature 100%
• Trace Elements 100%
• Miocene 100%
• Mantle Metasomatism 100%
• 206Pb 66%
• Isotope Ratio 66%
• Metasomatic 66%
• Chemical Composition 33%
• Phlogopite 33%
• Volcanic 33%
• Subduction 33%
• Isotopic Data 33%
• 207Pb 33%
• Potassium 33%
• Isotopic Composition 33%
• Andesite 33%
• Late Miocene 33%
• Western Anatolia 33%
• Basaltic Andesite 33%
• Rock Type 33%
• Isotope Pattern 33%
• Depleted Mantle 33%
• 208Pb 33%
• Subduction Events 33%
• Pb Isotopes 33%
• Lithospheric Mantle 33%
• Melt Metasomatism 33%
• Relative Abundance 33%
• RBS-R 33%
• Continental Lithosphere 33%
• Lava Flow 33%
• Crustal Origin 33%
• Subduction Signature 33%
• Geochemical Signature 33%
• Mantle Origin 33%
• U-Pb 33%
• Role of Water 33%
• Devolatilization 33%
• Mantle Peridotite 33%
• Number of Individuals 33%
• Subducted Sediment 33%
• Differential Effects 33%
• Isotopic Evolution 33%
• Derived Material 33%
• Elemental Abundances 33%
• Isotopic Diversity 33%

Earth and Planetary Sciences

• Miocene 100%
• Metasomatism 100%
• Trace Element 100%
• Andesite 66%
• Isotopic Ratio 66%
• Phlogopite 33%
• Peridotite 33%
• Isotopic Composition 33%
• Continental Lithosphere 33%
• Lava Flow 33%
• Isotope Ratios 33%