Origin and evolution of overlapping calc-alkaline and alkaline magmas: The Late Palaeozoic post-collisional igneous province of Transbaikalia (Russia)

Keyphrases

• Alkali Feldspar 25%
• Alkaline Granite 25%
• Alkaline Magmas 100%
• Alkaline Syenite 25%
• Alkalinity 25%
• Angara 25%
• Basalt 50%
• Batholith 50%
• Calc-alkaline 100%
• Calc-alkaline Granitoids 75%
• Closely Spaced 25%
• Convection-diffusion 25%
• Diffusion Model 25%
• Equal Ratios 25%
• Fractional Crystallization 50%
• Generation Process 25%
• Geochemical Data 25%
• Granitoids 50%
• High-K Calc-alkaline 25%
• High-K Calc-alkaline Granite 50%
• Highly Alkaline 50%
• Hybrid Magma 25%
• Igneous Province 100%
• Lake Baikal 25%
• Large Region 25%
• Late Paleozoic 100%
• Low Silica 25%
• Lower Crust 25%
• Mafic Magma 25%
• Mafic Rocks 25%
• Magma 100%
• Magma Generation 25%
• Magma Mixing 25%
• Magmatic Activity 25%
• Magmatism 25%
• Mantle-derived 50%
• Metamorphic Rocks 25%
• Monzonite 50%
• Partial Melting 25%
• Partially Overlapped 25%
• Peralkaline 25%
• Post-collision 100%
• Quartz Syenite 50%
• Relative Contribution 25%
• Rift 25%
• Selenga 50%
• Silicic 25%
• Silicic Magma 25%
• Sr-Nd-O Isotopes 25%
• Supracrustal 25%
• Syenite 50%
• Transbaikalia 100%
• Within-plate 50%

Earth and Planetary Sciences

• Alkali Feldspar 11%
• Alkalinity 11%
• Basalt 22%
• Batholith 22%
• Fractional Crystallization 22%
• Granitoid 55%
• Igneous Province 100%
• Lower Crust 11%
• Mafic Rock 11%
• Magma 100%
• Magma Generation 11%
• Magmatism 11%
• Metamorphic Rock 11%
• Monzonite 22%
• Paleozoic 100%
• Partial Melting 11%
• Russia 100%
• Syenite 55%
• Territory 11%