The Evolution of the Igneous Rocks
Quick Summary
Norman L. Bowen's work on igneous rocks, particularly his reaction series, explains how minerals crystallize from cooling magma. The series is divided into two branches: a discontinuous series where minerals like olivine transform into new minerals as temperature drops, and a continuous series where plagioclase feldspar changes composition.
These reactions are crucial because early-formed, high-temperature minerals can react with the remaining liquid magma to form new minerals as it cools. If these early crystals are removed, such as by gravity, the magma can evolve into rocks with different mineral compositions. This process, known as fractional crystallization, helps explain the diversity of igneous rocks like basalt, andesite, and granite, which form at different temperature ranges and have varying silica content.123
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