Concept:
Bowen’s Reaction Series describes the order in which minerals crystallize from a cooling magma. As magma cools, minerals form at different temperatures depending on their chemical composition.
The series is divided into two main branches:
- Discontinuous series: Olivine → Pyroxene → Amphibole → Biotite
- Continuous series: Calcium-rich plagioclase → Sodium-rich plagioclase
Minerals at the
top of the series crystallize at the highest temperatures. Minerals toward the bottom crystallize at lower temperatures.
Step 1: Understanding the highest temperature mineral.
At very high temperatures (about \(1200^\circ C\)), the first mineral to crystallize from a cooling silicate magma is
Olivine. It is rich in magnesium and iron and forms early during magma cooling.
Step 2: Position of other minerals in the series.
- Quartz: Crystallizes at the lowest temperatures.
- Biotite: Forms later in the discontinuous branch.
- Muscovite: Forms at relatively low temperatures.
Since
Olivine crystallizes first at the highest temperature, it is the correct answer.