Answer:
The best answer for the given question out of the four options provided is
option C.
Explanation:
Decompression melting also known as adiabatic melting of the mantle is most commonly linked with divergent boundaries of the plate, which serves as the point of the 2 tectonic plates from one another along a mid ocean ridges leading to the generation of magma.
Therefore, thinning of Lithosphere at diverging boundaries , allows hot mantle rocks to melt as a result of decompression.