IGNEOUS PROCESSES Flashcards
- Describe the rock cycle, the driving forces, and basic formation of each rock type
o Rocks- consolidates mixtures of mineral
o Igneous
Formed from crystallization of magma
o Sedimentary
Formed from weathered fragments of other rocks
Fragments are buried, compresses and consolidates
o Metamorphic
Formed by temp, pressure, fluids and time
o The rock cycle
Can start anywhere and any rock can transform into another, except sedimentary rocks don’t transform into igneous because they have to become metamorphic first
o Lava
Molten rock above the ground
magma
Molten rock below the ground
Types
* Crystal (solid)
* Melt (liquid)
* Volatiles (gas)
Dominated by silicon and oxygen
* The more silicon the more felsic
- Differentiate extrusive and intrusive igneous rocks
o Intrusive plutonic-magma slowly cools below the surface
Large crystals
o Extrusive/ volcanic- magma cools quickly above the surface
Small/no crystals
o Partial melting
All magmas are derived from partial melting of rock in the mantle or crust
Rocks are made form different minerals
Minerals melt at different temps
Temps rarely exceed that of all mineral’s melting point
This result in only part of rock melting
o Ways to make magma
Increase temp
Decrease pressure (decompression melting)
* Decrease pressure while maintaining temp
* At divergent boundaries mantle rock rises in response to the newly created space
* The mantle rocks rise and are kept at approx same temp, but reduce pressure, inducing melting
* Hot spots (mantle plume) are deep magmas from deep within the mantle
* As the plume rises it continues melting due to decreases in pressure
Add water or other volatiles (flux melting)
* Adding volatiles lowers the melting point of rocks
* Liquidus curve shifts left
* At convergent boundaries where subduction occurs water is released into he mantle from the subducting slab
* The added water (volaties) lower the melting point of the mantle rock
Tectonic summary for melting
Most melting is controlled by plate tectonics
- Know the broad classification of chemical compositions of magma
mafic - 50 % Sio2, least Na2O, most Al2O3, most FeO
felsic- 75% Sio2, most in Al2O3
intermediate- 55% SiO2
- Explain how magma and rock composition is influences by partial melting and fractional crystallization
crystallization of magma, the sequence of crystallization: Bowen’s reaction series
fractional crystallization
o Crystallization of magma
Rock crystalizes at different temps depending on mineral composition
Minerals crystalize at different temps
o The sequence of crystallization: Bowen’s reaction series
More mafic crystalize first
Plagioclase crystallizes around the same temp as procxene but depends on the plagioclase composition
* Ca rich (Anorthite) Na rich (Albite) K rich (K-spar
o Fractional crystallization
The consequence of bownes Rxn series is that as magmas cool, mafic minerals crystalize first, making the magma composition more felsic
- Differentiate dikes and sills
o Depending on how tabular bodies of magma interact with surface statigraphy, they are either dikes or sills
sill
Concordant (parallel) with existing laying
dike
If there is no layer present