METAMORPHIC PETROLOGY (FUNDAMENTALS) Flashcards

1
Q

This refers to predominantly solid state mineral and/or textural changes to preexisting protoliths
“to change form” a process that leads to changes in mineralogy, texture, and sometimes chemical composition

A

Metamorphism

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2
Q

Agents of metamorphism

A

1.Temperature,
2.Pressure,
3.chemically active fluid
4. Differential stress*

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3
Q

Types of metamorphism which results from INCREASING T and P consitions overtime w/c involces recyrstallization and neocrystallizaton to transform minerals in accordance with equilibrium

A

Prograde Met

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4
Q

Type of Metamorphism which results to DECREASE T and P so that lower T/P minerals OVERPRINTS unstable ones with the AID OF VOLATILES

A

Retrograde Met

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5
Q

Type of Met which progresses incrementaly from slight changes

A

Low-grade Met

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6
Q

Type of Met which progresses incrementaly showing substantial changes

A

High-grade Met

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7
Q

Determine if its Retrograde or Prograde
1. Neocrystallization
2. Overprinting with aid of volatiles
3. Recrystallization

A
  1. PM
  2. RM
  3. PM
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8
Q

Differentiate Prograde and retrograde metamorphism

A

Prograde metamorphism results from increasing temperature and pressure conditions over time which involves recrystallization and neocrystallization to transform minerals in accordance with equlibrium meanwhile Retrograde metamorphism occues when temp and pressure conditions decreases so that lower temp/press minerals overprints unstable minerals with the aid of volatiles

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9
Q

This involves the use of mineral assemblages and their deformation chatacteristics to infer peak PT conditions of metamophism

A

Geothermobarometry

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10
Q

This mineral occurs in LT HP in subduction zones

A

Glaucophane

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11
Q

lower limits of metamorphism

A

Diagenesis
150-200 deg cel
<3kbar
10km depth

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12
Q

Temp limit of diagenesis

A

150-200 deg cel

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13
Q

Pressure limit of diaganesis

A

<3Kbar

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14
Q

Depth limit of Diagenesis

A

10 km

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15
Q

Upper limits of metamorphism

A

Anatexis (Partial melting) (600-800deg)

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16
Q

this occurs when bulk composition of rocks changes as a result of chemical reactions with hot chemically active fluid of variable origin

A

Hydrothermal Alteration

17
Q

What are the anions or cations which serves as catalyts in hydrothermal alteration

A

H2O, CO2, CH4, K, Na, B, S, Cl

18
Q

Fluids derived principally from magma at oceanic spreading ridges, magmatic arcs or hotspots

A

Juvenile or magmatic fluids

19
Q

This infiltrates fractures and pore spaces at ocean spreading ridges and subduction zones

20
Q

These are fluids derived from subduction zones which releases H2O from mica, amphibole and Serpentine and CO2 from limestone and dolostones

A

Devolatilization-derived fluids

21
Q

Associated with precipitation, surface water, and groundwater

A

Meteoric Fluids

22
Q

fluids which are stored in spaces between cyrtslas

A

Connate fluids

23
Q

Another name for connate fluids

A

Formation Pore Fluids

24
Q

What are the indicators of metamorphism by chemically active fluid?

A

1)Presence of Volatile rich minerals
2) Secondary Mienerals in vein fillings and fluid inclusions

25
Common metamorphic minerals in increasing temparature stability
Chlorite - Muscovite - Biotite - Garnet - Staurolite - Kyanite - Sillimanite
26
Two processes which promotes Hydrothermal Alteration
1) Deuteric Reactions 2) Metasomatic Reactions
27
These involves reactons in which igneous rocks are metamorphosed due to its own hot-vapor-rich fluids "Ginigisa sa sariling Mantika"
Deuteric Reactions
28
deuteric reaction of micas results to
Chlorite
29
deuteric reaction of clay results to
Sericite
30
deuteric reaction of plag results to
Epidote
31
This involves changes in solid rock compostion resulting from hydrothermal fluids exchanging components with an external source
Metasomatism
32
The process in which ca plag turns to na plag when basaltic magma reacts with Na rich saltwater
Spilitization
33
A process whereby elements are removed from the rock by during hydrothermal alteration
leaching
34
Sites of metallic mineral deposit due to metasomatic processes
Oceanic Crust and Ophiolites
35
Ore metals formed by metasomatic process in the ocean floor
Co, Cu, Mn
36
Differentiate uniform from non-uniform stress
Uniform stress aka isotropic stress, lithstatic pressure or hydrostatic pressure or confining pressure is associated with burial depth in which forces are equal or of the same magntude in all directions thus producing dilation but not distortion in shape. While non-uniform or anisotropic or deviatoric stress forces varies with direction
37
What rocks are produced by uniform stress?
Non-foliated met rocks with equant grains
38
What rocks are produced by non uniform stress?
Inequant grains and foliated met rocks
39
A metamorphic layering developed due to preferred aligned arrangement of inequant grains
Foliation or Foliated texture