Step 1: Understand the discontinuous branch of Bowen's reaction series.This series details the crystallization temperatures of silicate minerals from cooling magma, with the discontinuous series focusing on ferromagnesian minerals.
Step 2: Order the minerals in the discontinuous series by decreasing crystallization temperature.The order is:1. Olivine (e.g., Forsterite, D) - Highest Temperature2. Pyroxene (e.g., Clinopyroxene, B)3. Amphibole4. Biotite mica (A) - Lowest Temperature
Step 3: Determine which minerals crystallize before amphibole.Olivine (Forsterite) and Pyroxene (Clinopyroxene) crystallize before amphibole.
Step 4: Examine other minerals.- Biotite (A) crystallizes after amphibole.- K-feldspar (C) from the continuous branch crystallizes at lower temperatures than amphibole.Conclusion: Clinopyroxene (B) and Forsterite (D) crystallize before amphibole.