Difficulty: Easy
Correct Answer: Bowen's reaction series
Explanation:
Introduction / Context:
As magma cools, minerals crystallize in a predictable order. This order controls the evolving composition of the remaining melt and thus the rock types produced. Understanding this sequence is foundational in igneous petrology.
Given Data / Assumptions:
Concept / Approach:
Bowen’s reaction series depicts discontinuous and continuous branches: olivine → pyroxene → amphibole → biotite (discontinuous), and plagioclase evolving from Ca-rich to Na-rich (continuous). As crystallization proceeds, magma composition shifts from mafic to felsic, explaining basalt, andesite, dacite, and rhyolite generation pathways.
Step-by-Step Solution:
Identify the need: a crystallization-order model.Recall Bowen’s series as the specific petrologic diagram for this purpose.Contrast with the rock cycle, which is a high-level transformation loop among igneous, sedimentary, and metamorphic rocks.Select Bowen’s reaction series.
Verification / Alternative check:
Introductory geology textbooks universally present Bowen’s series to explain fractional crystallization and the derivation of igneous rock suites.
Why Other Options Are Wrong:
Rock cycle — too general; not a crystallization sequence model.Both are similar — false; they address different scales.None — incorrect since a well-known model exists.Plate-tectonic cycle — addresses crustal recycling, not mineral order.
Common Pitfalls:
Confusing broad Earth cycles with specific igneous processes. The keyword is “crystallization sequence.”
Final Answer:
Bowen's reaction series
Discussion & Comments