Consider a schematic isobaric ternary phase diagram A-B-C, shown below, which is contoured with isopleths of liquidus temperatures (in \(^\circ C\)), reveals crystallization behaviour of melt (L) of different compositions during cooling. When a melt of composition "a" lies at a temperature of 1800\(^\circ C\), the variance (or degree of freedom) of the magmatic system is ........
