Geochemistry
Subduction zones are areas where one tectonic plate is being forced beneath another, leading to the recycling of the oceanic lithosphere into the mantle. These zones are crucial for understanding geological processes such as the formation of mountain ranges, volcanic activity, and earthquakes. The interaction between the descending plate and the surrounding materials significantly impacts the composition and behavior of the crust and mantle, influencing magma generation and metamorphic processes.
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