Petrographic Texture Flashcards

1
Q

Phenocrysts lie in a matrix of glass

A

Vitrophyric

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2
Q

Groundmass is a dense overgrowth of quartz and feldspar

A

Felsophyric

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3
Q

Groundmass is made up of rectangular formed feldspar instead of lath slender lath crystals

A

Orthophyric

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4
Q

Phenocrysts in a porphyritic texture are clustered into aggregates called glomerocrysts or crystal clots which indicates crystal fractionation by crystal settling

A

Glomeroporphyritic

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5
Q

Phenocrysts contain small grains of other minerals, enclosing them, indicating that the smaller grains may have crystallized first.

A

Poikilitic

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6
Q

Variety of poikilitic texture where plagioclase laths are enclosed by pyroxenes or olivine.

A

Ophitic

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7
Q

Variety of Ophitic wherein plagioclases enclose ferromagnesian minerals, indicating slower cooling in basaltic rocks

A

Subophitic

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8
Q

Angular interstices between feldspars filled with glass Instead of pyroxene

A

Hyalophitic

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9
Q

Also called corona, reaction rim and Rapakivi, displays a secondary mineral formed around another mineral, indicating a post-magmatic reaction

A

Opacitic

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10
Q

Variety of opacitic where there is a secondary rim or corona

A

Kelyphitic

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11
Q

Occurs where crystal occupies occupy spaces between at least two larger crystals, indicating a later formation

A

Intergranular

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12
Q

Denotes that angular spaces between crystals are filled with glass, that may be devitrified or altered, and small crystals

A

Intersertal

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13
Q

Holocrystalline groundmass with lath-shaped microlites, typically plagioclase, are generally oriented irregularly

A

Pilotaxitic

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14
Q

Extrusive igneous rock texture wherein the groundmass flow in the direction of lava flow and around inclusions, and occurs in alkali-rich rocks

A

Trachytic

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15
Q

Macroscopic variety of Trachytic that is visible to the naked eye

A

Trachytoid

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16
Q

Or Symplectic, is an intergrowth of branching rods of quartz set in a single crystal of plagioclase

A

Myrmekitic

17
Q

Observed where a solid solution phase unmixes into two separate phases in the solid state, often occurring between two or more endmember compositions

A

Exsolution

18
Q

Intergrowth of plagioclase feldspar in alkali feldspar host

A

Perthitic

19
Q

Intergrowth of alkali feldspar in plagioclase feldspar host

A

Holocrystalline

20
Q

Contains 100% crystals

A

Hypocrystalline

21
Q

A mix of glass and crystals, but contains more crystals than glass

A

Hypohyaline

22
Q

contains 100% glass

A

Holohyaline / Vitric

23
Q

Contains very coarse grains having >30mm in diameter

A

Pegmatitic

24
Q

contains coarse-grained minerals

A

Phaneritic / Dyscrystalline

25
Q

contains fine-grained minerals

A

Aphanitic / Eucrystalline

26
Q

Too fined-grained to be distinguish minerals microscopically

A

Cryptocrystalline

27
Q

Displays grains that are generally equant

A

Granular

28
Q

Medium- to coarse-grained minerals, most of which are devoid of crystal faces

A

Granitic

29
Q

Contains equidimensional cryptocrystalline groundmass

A

Felsitic

30
Q

Variety of Poikilitic where in inclusions have a complete series of crystal sizes

A

Seriate