Linked from

The 20 pages that link to Bowen's reaction series, each with the reason it gives.

• Silicate mineralRelated: Its sequence links silicate composition and structure to crystallization conditions.

• GraniteRelated: It helps explain why granite’s minerals crystallize from evolved, relatively cool magma.

• Igneous rockRelated: Its crystallization sequence helps explain igneous mineral assemblages.

• FeldsparRelated: Feldspar types help mark magma crystallization conditions in this sequence.

• PlagioclaseRelated: Its continuous branch tracks changing plagioclase composition during magma cooling.

• Crystal fractionationRelated: Fixes which minerals settle out at each temperature, setting the melt's changing path.

• GabbroRelated: It explains why pyroxene and calcium-rich plagioclase crystallize from hot mafic magma.

• AlbiteRelated: Puts albite at the low-temperature end of the plagioclase limb, where this page's story lands.

• Igneous petrologyRelated: It links changing magma temperature to mineral assemblages in igneous rocks.

• Alkali feldsparRelated: Alkali feldspar typically crystallizes late from evolved, silica-rich magmas.

• Intrusive rockRelated: It links cooling conditions to the minerals found in intrusive rocks.

• Phaneritic textureRelated: Mineral assemblages in coarse-grained rocks can be interpreted alongside crystallization order.

• DioriteRelated: It explains why diorite’s plagioclase and dark minerals crystallize at different stages.

• Skaergaard intrusionRelated: Bowen’s predictions gave researchers a framework for interpreting the intrusion’s mineral sequence.

• Ultramafic rockRelated: Its early-forming olivine and pyroxene help explain ultramafic mineral assemblages.

• GranodioriteRelated: It explains how feldspars and quartz can crystallize in granodioritic magma.

• AugiteRelated: Augite crystallizes over a range of conditions in the mafic part of the series.

• Extrusive rockRelated: It connects cooling history and magma composition to minerals in volcanic rocks.

• Igneous differentiationRelated: Its crystallization sequence predicts which elements early minerals remove from melt.

• Plagioclase feldspar solid solution seriesRelated: The plagioclase branch is the continuous arm of Bowen's two-branch scheme.