Concept:
Bowen's Reaction Series explains the sequence in which minerals crystallize from a cooling magma. It is divided into two branches:
- Discontinuous series: Minerals change structure as temperature decreases (Olivine $\rightarrow$ Pyroxene $\rightarrow$ Amphibole $\rightarrow$ Biotite).
- Continuous series: Plagioclase feldspar evolves gradually from calcium-rich to sodium-rich composition.
The discontinuous series is called so because each mineral has a different crystal structure and forms at different temperature ranges.
Step 1:Identify the highest temperature mineral in the discontinuous series.
Minerals crystallize from magma as it cools, with high-temperature minerals forming first.
Step 2:Recall the order of the discontinuous series.
\[
\text{Olivine} \rightarrow \text{Pyroxene} \rightarrow \text{Amphibole} \rightarrow \text{Biotite}
\]
Step 3:Determine the first crystallizing mineral.
Olivine forms at the highest temperature and is therefore the first mineral to crystallize in the discontinuous series.