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In mid-ocean ridges, intraoceanic island-arcs and oceanic islands, magmas can only be generated at the upper mantle due to the absence of continental crust. On the contrary, the crust can play an important role in continental settings. Additionally, the generation of magma in the upper mantle can be located in the asthenosphere and the lithosphere. The mechanisms of magma generation in each geodynamic setting is different. In constructive plate margins, the asthenosphere rises adiabatically and melts. In destructive margins, melting is linked to subduction. Finally, in continental intraplate areas melting is associated to extensional processes, which can be linked to various phenomena such as indentation, delamination or mantle plumes, as in the case of oceanic intraplate settings. The eruptive mode depends strongly on the magma composition, and more precisely of its temperature, viscosity and gas content. 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