IGNEOUS PROCESSES Flashcards

1
Q
  • Describe the rock cycle, the driving forces, and basic formation of each rock type
A

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

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2
Q

o Lava

A

 Molten rock above the ground

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3
Q

magma

A

Molten rock below the ground
 Types
* Crystal (solid)
* Melt (liquid)
* Volatiles (gas)
 Dominated by silicon and oxygen
* The more silicon the more felsic

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4
Q
  • Differentiate extrusive and intrusive igneous rocks
A

o Intrusive plutonic-magma slowly cools below the surface
 Large crystals
o Extrusive/ volcanic- magma cools quickly above the surface
 Small/no crystals

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5
Q

o Partial melting

A

 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

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6
Q

o Ways to make magma

A

 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

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7
Q

Tectonic summary for melting

A

 Most melting is controlled by plate tectonics

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8
Q
  • Know the broad classification of chemical compositions of magma
A

mafic - 50 % Sio2, least Na2O, most Al2O3, most FeO
felsic- 75% Sio2, most in Al2O3
intermediate- 55% SiO2

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9
Q
  • Explain how magma and rock composition is influences by partial melting and fractional crystallization
A

crystallization of magma, the sequence of crystallization: Bowen’s reaction series
fractional crystallization

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10
Q

o Crystallization of magma

A

 Rock crystalizes at different temps depending on mineral composition
 Minerals crystalize at different temps

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11
Q

o The sequence of crystallization: Bowen’s reaction series

A

 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

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12
Q

o Fractional crystallization

A

 The consequence of bownes Rxn series is that as magmas cool, mafic minerals crystalize first, making the magma composition more felsic

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13
Q
  • Differentiate dikes and sills
A

o Depending on how tabular bodies of magma interact with surface statigraphy, they are either dikes or sills

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14
Q

sill

A

 Concordant (parallel) with existing laying

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15
Q

dike

A

 If there is no layer present

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16
Q
  • Identify plutons based on morphology and relation to surrounding rocks
A

o Any body of magma that crystalizes underground is a pluton
o They can be divided by shape and size
 Stocks/ batholiths
* Large pluton (>100km2) usually formed by several stocks merging together
 Sills
 Fyke
 Laccolith
* Mushroom shaped body of magma that inflates between layers, moving them upwards
 Volcanic pipe

17
Q

o Texture of rocks is a result of the crystallization process or the eruptive style of the volcano

A

 Glassy
 Porphyritic texture
* Two distinctly different crystal sizes
 Phaneritic (coarse-grained) texture
* Large mineral grains
 Vesicular texture (pumice)
* Extrusive rock containing voids by gas bibbles
 Pyroclastic (fragmental) texture
* Produced by the consolidation of fragments (ash, once molten blobs or large angular blaocks) that were ejected by volcdanic eruption
 Aphanitic (fine grained) texture

18
Q
  • Classify igneous rocks using basic terms to describe composition and texture
A

o Porphyritic texture
 After minerals crystalize in the magma, and are brought up to the surface, the lava will quench and from a porphyritic texture
o The more mafic the rock the higher portion of ferromagnesian minerals it contains

19
Q
A