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Bowen

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Bowen s Reaction Series What is Bowen s Reaction Series? Bowen s Reaction Series helps us understand why certain types of minerals tend to be found together ... – PowerPoint PPT presentation

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Title: Bowen


1
Bowens Reaction Series
What is Bowens Reaction Series? Bowens Reaction
Series helps us understand why certain types of
minerals tend to be found together while others
are almost never found together.
  • How Does It Work?
  • Different minerals form from magma at different
    temperatures.
  • Some minerals crystallize when magma is at a
    higher temperature, while others only crystallize
    when magma is at a lower temperature.
  • Minerals that form at high temperatures are
    listed at the top and minerals that form at lower
    temperatures are listed at the bottom.
  • Rocks that form from magma at high temperatures
    are called mafic and tend to be dominated by dark
    colored minerals such as olivine and pyroxene.
  • Rocks that form from magma at lower temperatures
    are called felsic and tend to be dominated by
    light colored minerals such as potassium feldspar
    and quartz.



Muscovite
Pyroxene
Olivine
Biotite
Potassuim Feldspar
Amphibole
Quartz
Mafic
Felsic
2
Bowens Reaction Series


What is Bowens Reaction Series? Bowens Reaction
Series helps us understand why certain types of
minerals tend to be found together while others
are almost never found together.
  • How Does It Work?
  • Different minerals form from magma at different
    temperatures.
  • Some minerals crystallize when magma is at a
    higher temperature, while others only crystallize
    when magma is at a lower temperature.
  • Minerals that form at high temperatures are
    listed at the top and minerals that form at lower
    temperatures are listed at the bottom.
  • Rocks that form from magma at high temperatures
    are called mafic and tend to be dominated by dark
    colored minerals such as olivine and pyroxene.
  • Rocks that form from magma at lower temperatures
    are called felsic and tend to be dominated by
    light colored minerals such as potassium feldspar
    and quartz.
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