METAMORPHIC PETROLOGY (ZONE, FACIES, SERIES) Flashcards

1
Q

Temperature of metamorphism

A

150-600

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2
Q

Subdvisions of Metamorphism temperature

A

L: 150-400
M:400-600
H:>600

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3
Q

Subdivisions of Metamorphic Pressyre

A

L: 0-2 Kbar = 0-6 km
M: 2-6 Kbar = 6-20 km
H: >6kbar = >20km

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4
Q

3.3 Kbar is equivelent to what depth?

A

approx. 10km

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5
Q

Max depth of metamorphism

A

40-50 Km

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6
Q

Minerals that form within a more limited temperature and/or pressure range which effectively indicate the temp/pressure conditions of metamorphism occuring in such environment

A

Index Minerals

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7
Q

Index minerals of Barrow and Tilley

A

Chlorite
Biotite
Almandine
Staurolite
Kyanite
Sillimanite

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8
Q

Lines drawn on geologic maps that mark the FIRST APPREANCE of a particular index mineral

A

Isograds

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9
Q

Regions bounded by two isograds of an index mineral

A

Metamorphic Zone

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10
Q

This is the six metamorphic zones based on the six index mineral isograds which is a key to interpret progressive metamorphism in an evolving orgenic belt

A

Barrovian Zones

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11
Q

Who first characterized Metamorphic zones

A

George Barrow and
C.E Tilley
Harker
Scotland

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12
Q

Biotite forms from what minerals

A

Chlo
Musc
Qtz
Ruti
Magn

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13
Q

In Almandine Zone, garnet usually occurs as?

A

Porphyroblasts

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14
Q

Minerals which transform to almandine

A

Chlo and Magnetite

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15
Q

Lower Temp minerals in Barrovian Zones

A

Chlorite, Biotite, Almandine

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16
Q

High Temp minerals in Barrovian Zones

A

Staurolite, Kyanite, Sillimanite

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17
Q

Kfelds form from the breadkdown of what mienral?

A

Muscovite

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18
Q

Stauroilite forms from what minerals?

A

Almandine, Chlorite and Muscovite

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19
Q

staurolite exists only in?

A

Staurolite Zone

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20
Q

High Pressure aluminosilicate?

A

Kyanite (Al2SiO5 or Al AlO SiO4)

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21
Q

Low Pressure aluminosilicate

A

Andalusite

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22
Q

dehydration of these minerals form Kyanite

A

Staurolite and Pyrophyllite

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23
Q

Marks the highest temperature zone defined by Barrow and Tilley

A

Sillimanite Zone

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24
Q

High Temp Alumino silicate?

A

Sillimanite

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25
Sillimanite can form from dehydration of this mineral in the presence of Quartz
Muscovite
26
Barrovian Zones are based on the observation of what kind of met rocs
Pelitic
27
Whats the limitations of Barrovian Zones
Cannot be used in non-peilitic not compatible for subduction settings non compatible for contact Met Envi
28
Distinctive mineral Assemblages in met rocks that form in response to a particular range of temperature and/or pressure conditions and does not imply genetic origin but assemblages closely constrains the temp and/or pressure condtitions
Metamorphic Facies
29
Who first describe metamorphic facies?
Pentii Eskola, Finland
30
Give the Metamorphic Facies in Increasing TandP
Alb-Epi Horn Hbl Horn Pyx Horn Sanidinite Horn Zeol Prehnite-Pumpelly Greensch Ampihbo Granu Blue Sch Eclogite
31
The Hornfels facies are subdivided into how many subfacies?
four Albite-Epid Hbl, Pyx, sanidinite
32
Type of met that produces hornfels
Heat induced in areas with igneous intrusions Contact Met or Hydrothermal Met
33
Environment where hornfels usually form
Ocean Spreading Centers which represent hydrothermal met
34
What defines a particular hornfels facies?
Non-foliated Texture and Index Mineral Assemblage
35
In Hornblende Facies, at 450deg cel. Dolomite is replaced by this mineral
Diopside
36
Hornfels facies record what
Temp driven minreal changes driven by igneous intrusions into country rock or hydrothermal metamorphism related to shallow magmatc activity
37
at which depth does Contact Metmorphism predominates
upper 10 km
38
In what TandP range does Zeolite and Prehnite-Pumpellyite form
Low to Mod Tand P
39
What type of Metamorphism is responsible to zeolite and prehnite-pumpellyite
Burial Met in Sed Basins as well as at Hydro Met at Ocean Ridges, Hotspots and Volcanic Arcs
40
Low temp low press met series
Zeolite Facies
41
Hydrous Na and Ca Al tectosilicates forme by diagenetic and low temp metamorphic rections
Zeolites
42
Possible origins of Zeolite Facies Minerals
1)Hydro. Alt of Volcanic Protolith 2) Devitrification of Basalat Glass and Tuff 3) Reaction of Pelite and Graywacked with Saline Water
43
Where do Zeolite minerals usually occur or mode of occurrence
Isolated Vesicles and Veins Disseminated within met rocls
44
series of alteration of Zeolite minerals in increasing T and P
Stilbite - Heulandite - Laumontite - Wairakite
45
at what temp do zeolite minerals alter to prehnite pump
250deg cel 3-5km
46
High temp alteration of Prehnite-Pumpellyite results in the neocrystallization of these minerals which also marks the boundary towards Albite-Epidote Hornfels Series and greenschist facies
Actinolite and Epidote
47
High T and High P met facies are produced by
Dynamothermal under non-uniform stres
48
Environment of formation of HiT-P met facies
Convergent plate
49
Barrovian Zones that corresponds to Greenschist Facies with Pelitic Protolith
Chlotie Zone - Lower Gschist Facies Biotite Zone - Upper facies L.Almandine Zone - Uppermost
50
What marks the transition from Greenschist to Amphibolite facies
Inc: Hbl-Gnt-Antrhopyllite Dec: Acti-Chlo-Biotite-Talc
51
In what facies do staurolite appear in Pelitic rocs
Amphibolite
52
Hypersthene Bearing Granitic Gneiss
Charnockite
53
What separates Granulite I to granulite II
Presence of Hornblende and Biotite
54
Pyroxenes which only appears in Granulite Facies
Hypersthene and Diopside
55
Unusually high pressure/temperature rations reflecting existense of unsually low geothermal gradients
Blueschist Facies
56
Line of equal temperature
Isotherm
57
at which temp and pressurre does the Blueschist-greenschist transition facies occue
T: 350-450 P: 8Kbar
58
Minerals occur in Eclogite Facies at pressure >25 Kbar >80Km and Temp >600 deg cel
Ultra High Pressure Mineral
59
A high pressure polymorph of Silica
Coesite
60
High pressure polymorph of Carbon
Diamond
61
High Presure Garnet
Majorite
62
Crater at which coesite was first discovered
Meteor (Barringer)Crater
63
A sequence of facies that occurs across met terrane due to difference in PT conditions it provide key information concerning P-T-t conditions as well as Tectonic settings in which metamorphism occured
Metamorphic Facies Series
64
Three Major Group of Facies Series
Group
65
What kinds of rocks may be produced by low presure contact metamorphism
Hornfelsic and granoblastic
66
First Geologists who first mapped isograd zones in Scottish Highlands
George Barrow