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Igneous Processes ll Phil Simon A. Condat.

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Presentation on theme: "Igneous Processes ll Phil Simon A. Condat."— Presentation transcript:

1 Igneous Processes ll Phil Simon A. Condat

2 What is Magma -Molten or partially molten rock -silicate liquid
-carbonate and sulfide melts -lava

3 How does magma form Heat transfer Decompression melting
-upward movement -rises to an area of low pressure (convention) -overlying pressure/ decompression -divergent boundaries Heat transfer -hot, liquid rock intrudes into Earth’s cold crust -melts the surrounding rock -convergent boundaries Flux melting When H2O or CO2 are added to rock Rocks melt at lower temperature -subduction zones

4 Magmatic Differentiation
Minerals crystallize out of the melt - different ingredients separating suggestkeyword.com geologyclass.org

5 Magma mixing 2 or more magmas Different chemical compositions “Mix”
Compositions intermediate between end members basalt and rhyolite tend to inhibit mixing lavamagmainfo.weebly.com

6 Magma assimilation -Melts surrounding rocks
-Minerals become part of magma

7 Bowen’s Reaction Series
Norman L. Bowen (geologist) -”minerals crystallize differently as they cool.” sirismm.si.edu studyblue.com

8 Ultramafic – Fe, Mg. Ca Intermediate – combination
Continuous series Discontinuous series Residual phases Ultramafic – Fe, Mg. Ca Intermediate – combination Mafic – Fe, Mg, Ca Felsic – Si, Na,Al, K

9 References http://www.britannica.com/science/magma-rock#ref74566/
hedcenscience.wordpress.com

10 Thank you for listening!
maxisciences.com


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