Answer:
Option D
Explanation:
Bowen's reaction series arrangement can be described as a methods for positioning regular molten silicate minerals by the temperature at which they take crystallization occurs.
Minerals at the top have a comparatively high crystallization temperature, which implies that they will be the main minerals to take shape or to crystallize on cooling of the magma.
It also tends to give the explanation of magma type diversity and probable genetic relation among a variety of igneous rocks.
It provides a conceptualized framework on the basis of data from the lab experiments to interpret some of the connections in igneous rocks.