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Olivine Pyroxene Amphibole Biotite Plagioclase Feldspar Na-rich Ca-rich Potassium Feldspar Muscovite Quartz Felsic Intermediate Mafic Ultramafic cooling of magma 1400°C 700°C BOWEN’S REACTION SERIES Minerals crystallize out of magma and lava at various temperatures based on their composition and crystal structure. Bow- en’s Reaction Series was constructed by a Canadian geologist named Norman Bowen - a now famous geologist who used experiments to study how rocks and minerals form (a sub-field of geology called Petrology). Bowen’s Reaction Series is a widely used and refered to sequence in the geosciences that you should familiarize yourself with. Notice that each zoned area on the chart cooresponds to a specific set of minerals we associate with the igenous rock classifications ranging from felsic to ultramafic.

BOWEN’S REACTION SERIESdmaxbauer/3wk_Monday_Intrusive... · Erosion has removed part of the dike. Sill pushes between layers of rock. Dike cuts across layers. A..xock Dike A wall-like

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Olivine

Pyroxene

Amphibole

Biotite

Plag

ioclas

e Feld

spar

Na-rich

Ca-rich

Potassium FeldsparMuscovite

Quartz

Felsic

Intermediate

Mafic

Ultramafic

cool

ing

of m

agm

a

1400°C

700°C

BOWEN’S REACTION SERIESMinerals crystallize out of magma and lava at various temperatures based on their composition and crystal structure. Bow-en’s Reaction Series was constructed by a Canadian geologist named Norman Bowen - a now famous geologist who used experiments to study how rocks and minerals form (a sub-field of geology called Petrology). Bowen’s Reaction Series is a widely used and refered to sequence in the geosciences that you should familiarize yourself with. Notice that each zoned area on the chart cooresponds to a specific set of minerals we associate with the igenous rock classifications ranging from felsic to ultramafic.