IUGS Classification Coarse Grain/ Texture Flashcards

1
Q

Quartz compromise more than 90% of the felsic minerals, and has <90% mafic minerals. It may be hydrothermally altered granitoids (e.g. greisen)

A

Quartzolite

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2
Q

A light colored mineral where plagioclase is less than 10% of the total feldspar.

A

Alkali-feldspar granite

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3
Q

An alkali-feldspar/ total feldspar ratio from 0.35-0.90 on the QAFP diagram and 20 - 60% quartz

A

Granite

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4
Q

An alkali-feldspar/ total feldspar ratio from 0.65 - 0.90 and 20 - 60 quartz

A

Syenogranite

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5
Q

An alkali-feldspar/ total feldspar ratio from 0.35-0.65 on the QAFP diagram. Often called adamellite.

A

Monzogranite

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6
Q

It has 20-60% quartz and a plagioclase of 65-90% of the total feldspar.

A

Grandiorite

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7
Q

A granitoid, where plagioclase is >90%

A

Tomalite

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8
Q

Plagioclase is less than 10% of the total feldspar

A

Alkali-feldspar syenite

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9
Q

No quartz and containing up to 10% foids

A

Foid-bearing alkali feldspar syenite

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10
Q

Alkali-feldspar/ plagioclase ratio from 65-90% and <5% quartz. Intrusive equivalent of ‘trachyte’

A

Syenite

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11
Q

No quartz and <10% foids

A

Foid-bearing syenite

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12
Q

Equal amounts of alkali feldspar and plagioclase, and thus intermediate between diorite and syenite. Intrusive equivalent og latite.

A

Monzonite

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13
Q

Dioritic rock with <5% quartz and 10-35% alkali feldspar on the QAFP diagram.

A

Monzodiorite

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14
Q

A syenitoid with 5-20% quartz and subequal K-feldspar and plagioclase (35-65% of the feldspar being plagioclase). Coarse-grained equivalent of quartz-latite.

A

Quartz-monzonite

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15
Q

Less than 5% quartz or no foids, and no 10-35% K-feldspar.

A

Monzogabbro

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16
Q

Dioritic rock with 5-20% quartz and 10-35% alkali feldspar.

A

Quartz monzodiorite

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17
Q

More than 5% quartz and 10-35% K-Feldspar

A

Quartz monzogabbro

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18
Q

Foid-dioritoid where K-feldspar is >50-10% of feldspar

A

Foid monzodiorite

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19
Q

Foid gabbroic rock where plagioclase is 50-90% of feldspar

A

Foid monzogabbro

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20
Q

<5% quartz and <10% alkali feldspar on the QAFP diagram

A

Diorite

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21
Q

Composed of 10-90% Ca-dominant plagioclase and >5% clinopyroxene

A

Gabbro

22
Q

Mostly of calcic plagioclase (>90% usually labradiorite) with <10% mafics

A

Anorthosite

23
Q

Dioritic rock with 0-10% quartz and 10-35% alkali feldspar.

A

Quartz Diorite

24
Q

Gabbro with felsic minerals comprising more than 5% quartz

A

Quartz Gabbro

25
Q

Diorite with <10% foids and <10% alkali feldspar

A

Foid-bearing diorite

26
Q

Gabbro containing up to 10% foid minerals

A

Foid-bearing gabbro

27
Q

Rock where K-feldspar is >90%

A

Foid syenite

28
Q

Foid-syenitoid where K-feldspar is >50-90% of feldspar

A

Foid monzosyenite

29
Q

Foid-dioritoid where k-feldspar is 50-90%

A

Foid monzodiorite

30
Q

Plagioclase is >90% of feldspar

A

Foid diorite

31
Q

Rock with <90% mafics, >60% of felsic being foids

A

Foidolite

32
Q

Minerals consisting of aluminosilicates of sodium, potassium, or calcium and having too little silica to form feldspar.

A

Foids (feldspathoids)

33
Q

and Enumerate the common foid mineralss

A

Analcime
Leucite
Nepheline
Sodalite

34
Q

Crystals visible to the naked eye.

A

Phaneritic

35
Q

Crystals so small that they cannot be seen with the naked eye

A

Aphanitic

36
Q

Composed entirely of crystals

A

Holocrystalline

37
Q

Composed entirely of glass

A

Holohyaline

38
Q

Composed of crystal and glass

A

Hypocrytalline

39
Q

Phenocrysts set in a glassy groundmass

A

Vitrophyric

40
Q

Phenocrysts containing numerous inclusion of another mineral that they enveloped with growth.

A

Poikilitic

41
Q

Host crystal of poikilitc is termed as _________.

A

Poikilitc

42
Q

Holes in the rock formed by escaping gases during solidification

A

Vesicle

43
Q

Result of rapid growth of olivine and develop elongated olivine crystals

A

Spinifex texture

44
Q

Nucleation of one mineral on a preexisting mineral e.g. growth of sillimanite on biotite or muscovite

A

Epitaxis texture

45
Q

Plagioclase overgrowths on orthoclase (K-feldspar)

A

Rapakivi texture

46
Q

In silicic volcanic rocks in which needles of quartz and alkali feldspar growth radially from a common center

A

Spherulitic texture

47
Q

Refers to the envelopment of plagioclase laths by larger larger clinopyroxene and is commonly interpreted to indicate that clinopyroxene formed later.

A

Ophitic texture

48
Q

Radiating plagioclase laths in some basalts are probably the result of nucleation of later crystals on the first nuclei to form during devitrification of glass

A

Variolitic texture

49
Q

Evidence for advanced resorption, or rapid growth enveloping melt due to undercooling

A

Sieve texture

50
Q

Result from simultaneous crystallization of feldspar and quartz, the intergrowth forms epitaxially preexisitng phenocrysts or dikelet walls

A

Granophyre and Graphic Texture