Metamorphic reactions Flashcards

1
Q

How does mienrals respond to change of metamorphic conditions?

A

They go towrds equilibrium!
- minerals change
- metamorphic reactions happens

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2
Q

What are the most important metamorphic reactions?

A
  • Polymorphic transformations
  • Solid-solid nettransfer reaction
  • Devolatilization reactions
  • Continuous reactions
  • Ion exchange reactions
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3
Q

What is polymorphic reactions?

A

changes of solid minerals of same composition (polymorphs) only because of P or T changes

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4
Q

What is the catch with polymorphic reactions?

A

there is little potential energy for the reaction
- often end of as metastable (non-equillibrium assemblages)

ex. diamond brought to surface, doesn’t change to grafite

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5
Q

What is solid-solid nettransfer reactions?

A

Solids of different compositions.
Change in models amounts of the phase
(minerals react to create new minerals?)

if limited they are discontinuous
- line, and then new mineral (:)) by increase of T or P

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6
Q

What is Devolatilization reactions?

A

Reactions release or consume volatiles
- depends on P, T and Partial pressure of the volatile

  • very common
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7
Q

How does the devolitalization reaction affect the isograd?

A

i can make it move towrds lower temp. bc it is sensitive to the voltiles partial pressure

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8
Q

What types of devolatilization reactions are there?

A
  • Dehydration reaction (frees water)
  • Decarbonation reaction (frees CO2)
  • Combination (frees both)
  • Prograde reaction (either consumes water and frees CO2 or the opposite)
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9
Q

What is continuos reactions?

A

continually changing composition of phases bc. of the reaction
- Solid solution systems
- range of P and T

ex. breakdown of chlorite to get garnet,

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10
Q

Difference continiuous and discontiniuous reactions?

A

one changes apruptly to another mineral while the other is gradual change of the chemistry/composition of the phase

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11
Q

What is ion exchange reactions?

A

Reciprocal (gensidig) exchange of components between 2(+) minerals.

ex. Fe-Mg exchange between ortho- and clinopyroxene, or garnet and biotite

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12
Q

How is ion exchange different from continiuous reactions in the way it affect the cation ratios?

A

Ion exchange doesn’t change the modal composition of the phases - continiuous reactions does

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13
Q

What is the ideal form of Ion exchange reactions?

A

A(Fe) + B(Mg) = A(Mg) + B(Fe)

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14
Q

How can ploymorphic reactions be seen in compatibily diagrams?

A

Tie-lines does not change but a component (mineral) does

Reaction: Ky -> Si

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15
Q

What reactions can show crossing tie-lines in a compatibility diagram?

A

-Solid-solid nettransfer
-devolatilization
-continiuous

Reaction: Ms + Qtz -> Or + Sil (+ H2O)

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16
Q

What reactions can show terminal reactions in a compatibility diagram?

A

-Solid-solid nettransfer
-devolatilization
-continiuous

Reaction: Ms -> Or + Crn (+ H2O)
Cld ->Grt + ST + Chl

17
Q

How would ion-exchange reactions look in a compatibility diagram?

A

As rotating tie lines
(take up less or more space (chemical change) - angle changes)

18
Q

What is petrogenetic grids?

A

they show univarient reactions
- help define apperance/breakdown of key minerals (P-T range of assemblages)