Metamorphism of oceanic crust Flashcards

1
Q

What is the original rock type in oceanic crust?

A

Usually basalt

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2
Q

How are hydrous minerals formed?

A

Hydration of basalt, occur at any time, no need for deformation

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3
Q

Describe hydrothermal metamorphism

A

Cold seawater penetrates depths, replaced by hot fluid which returns to surface, creates convective scheme with large fluid volumes, significant retrogression occurs as crust moves away from heat

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4
Q

Name two common mineral alterations

A
Chlorite rich (Mg gain, Ca less)
Epidote rich (Ca gain, Mg less)
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5
Q

Where does subduction occur and how does it work?

A

Collision zones with old cold dense ocean lithosphere being taken to depth. Cold water taken to depth to creating large geothermal gradient

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6
Q

What two facies does subduction create?

A

Blueschist - (glaucophane)

Eclogite - (garnet and pyroxene)

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7
Q

How do blueschists form?

A

At depth with low geothermal gradient

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8
Q

How do blueschists reach surface?

A

Underplating of accretionary prism causes uplift of blueschist while keeping low geothermal gradient

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9
Q

What happens to blueschist during dehydration?

A

Transition to amphibolites and eclogites

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10
Q

What are eclogites normally made of?

A
Metabasic (garnet and pyroxene)
or Pelite (garnet, kyanite, Si rich white mica)
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11
Q

When do the three types of eclogites occur?

A

Xenoliths, high temp
blueschist dehydration, low temps
granulite or amphibolite facies, med temp, linked to crustal thickkening

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12
Q

What were crustal eclogites, what special mineral do they possess and how are they formed?

A

Originally basic intrusions, contain coesite which is a polymorph of quartz formed in deep subduction

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13
Q

What happened to eclogites on uplift?

A

Retrogressed to plag bearing gneisses

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14
Q

Explain the big density transitions that eclogites undergo

A

Rapid burial creates dense crustal root, delays uplift, slow heating, converts root to less dense rock, triggers uplift

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