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Fluid-induced melting refers to the process where the presence of fluids, such as water or other volatile substances, lowers the melting point of rocks or minerals, facilitating their transition from solid to liquid. This phenomenon often occurs in geological settings, such as subduction zones or magma chambers, where high pressure and temperature conditions prevail. The introduction of fluids can enhance the melting of rock by altering the physical and chemical properties of the minerals involved. This process plays a significant role in magma generation and the formation of igneous rocks.

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4d ago

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When is Fluid induced melting subducting plates?

Fluid-induced melting of subducting plates typically occurs at convergent plate boundaries, where one tectonic plate is forced beneath another. As the subducting plate descends into the mantle, it releases water and other volatiles, which lower the melting point of the overlying mantle wedge. This process leads to the generation of magma, contributing to volcanic activity associated with subduction zones. The melting is most pronounced at depths of around 100 to 200 kilometers, where the temperature and pressure conditions are suitable for such processes.


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