The ternary diagram given below shows phase relations for the Anorthite-Diopside-Forsterite system at 1 bar pressure. Broken lines represent isotherms with temperature in $^{\circ}\text{C}$. If 'P' is the initial melt composition, which one of the following is the CORRECT sequence of crystallization assuming equilibrium between crystal and melt?
The question requires understanding the crystallization sequence of the Anorthite-Diopside-Forsterite (An-Di-Fo) system at 1 bar pressure, starting from a specific melt composition labeled 'P' on the ternary phase diagram.
The correct crystallization sequence based on the phase diagram is: [Fo] → [Fo + An] → [Fo + An + Di].
Other options are incorrect because they involve crystallization sequences not supported by the phase regions crossed by the cooling path of the initial composition 'P'.
If 'X' represents the initial composition of a melt, which one of the trends indicated by arrows in the schematic diagram corresponds to the evolution of the residual melt composition during crystallization of diopside?
The diagram given below shows phase relations between components P and Q at 1 bar pressure. If ‘X' represents the initial liquid composition, which of the following statements is/are CORRECT during equilibrium crystallization?
The following diagram shows phase relations in a system consisting of components A and B at 1 bar pressure. If the initial composition of liquid is R, during cooling and crystallization of magma, which of the following statement(s) is/are CORRECT? 
The figure below represents an isobaric binary liquidus phase diagram, with the solid phases A, B and C. What are the degrees of freedom associated with equilibrium phase assemblages represented by the bulk compositions w, x, y and z, in the fields indicated in the figure?
