The Later Stages of the Evolution of the Igneous Rocks
Quick Summary
Norman L. Bowen's work, particularly his 1915 paper The Later Stages of the Evolution of the Igneous Rocks, revolutionized the understanding of how igneous rocks form from magma. He developed "Bowen's reaction series," which illustrates the sequence of mineral crystallization as magma cools.123
This series has two branches:
* Discontinuous series: Minerals like olivine transform into new minerals (pyroxene, amphibole, biotite) as temperature decreases.2
* Continuous series: Plagioclase feldspar changes composition from calcium-rich to sodium-rich as it cools.23
Fractional crystallization, where early-formed minerals are removed, is a key process that allows a basaltic magma to evolve into rocks with minerals found lower in the series, such as granite.2
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