Classification of Igneous rocks (composition) Flashcards

1
Q

How do we classify Igneous rocks?

A

Based on Composition
Based of Fabric and Texture
Base on Field relation

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2
Q

Most Straight forward approach to determining rock mineralogy that involves visually identifying the minerals and determining their percentage by volume.

A

Modal Composition or Mode

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3
Q

an indirect scheme using data derived from chemical analysis of a rock sample. this is commonly used in aphanitic or glassy volcanic rocks.

A

Normative Mineralogy

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4
Q

Why is Normative Mineralogy used in Aphanitc and glassy volcanic rocks?

A

because the modal mineral composition of these rocks can not be determined.

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5
Q

Rock group with <45% weighted percent silica (SiO2)

A

Ultrabasic

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6
Q

Rock group with 45-52% weighted percent silica (SiO2)

A

basic

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7
Q

Rock group with 52-66% weighted percent silica (SiO2)

A

Intermediate

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8
Q

Rock group with >66% weighted percent silica (SiO2)

A

Acidic (silicic)

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9
Q

Generally enriched in the elements iron and magnesium and are referred to as Ferromagnesian or Mafic minerals

A

Dark-colored Minerals

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10
Q

Depleted in Ferromagnesian elements and are generally enriched in elements such as silicon, oxygen, potassium, and sodium

A

Light-colored Felsic Minerals

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11
Q

Rocks that are Dark or greenish in color that’s rich in olivine and may or may not contain pyroxene or amphibole

A

Ultramafic

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12
Q

Dark-colored rocks containing pyroxene and amphibole. it may or may not contain some olivine and biotite

A

Mafic

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13
Q

Grayish to salt and pepper colored rocks rich in plagioclase and amphibole. It may or may not contain amounts of Biotite and Quartz.

A

Intermediate

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14
Q

Light-colored or red rock rich in potassium feldspar and quartz. It may or may not contain some amount of Biotite or Muscovite

A

Felsic

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15
Q

> 90% Dark-colored crystalline mineral

A

Ultramafic

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16
Q

70-90% Dark-colored crystalline mineral

A

Mafic

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17
Q

40-70% Dark-colored crystalline mineral

A

Intermediate

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18
Q

<40% Dark-colored crystalline mineral

A

Felsic

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19
Q

Quartz ± Feldspar and/or magnesium orthopyroxene

A

SiO2 oversaturated

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20
Q

Feldspar and/or Magnesium orthopyroxene only

A

SiO2 Saturated

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21
Q

Forsterite olivine, nepheline, leucite, and other feldspathoids ± feldspar and/or orthopyroxene minerals. excluding quartz

A

SiO2 undersaturated

22
Q

Forsterite olivine, nepheline, leucite, and other feldspathoids ± feldspar and/or orthopyroxene minerals. excluding quartz

A

SiO2 undersaturated

23
Q

<30% Dark Minerals according to Shand Classification

A

Leucocratic

24
Q

30-60% Dark Minerals according to Shand Classification

A

Mesocratic

25
60-90% Dark Minerals according to Shand Classification
Melanocratic
26
>90% Dark Minerals according to Shand Classification
Hypermelanic
27
<10% Dark Minerals according to Ellis Classification
Holofelsic
28
10-40% Dark Minerals according to Ellis Classification
Felsic
29
40-70% Dark Minerals according to Ellis Classification
Mafelsic
30
70-90% Dark Minerals according to Ellis Classification
Mafic
31
>90% Dark Minerals according to Ellis Classification
Ultramafic
32
Igneous rock based on AlO concentration: Al2O3 > CaO + Na2O +K2O
Peraluminous
33
Igneous rock based on AlO concentration: Al2O3 = Na2O +K2O
Subaluminous
34
Igneous rock based on AlO concentration: Na2O +K2O < Al2O3 < CaO + Na2O +K2O
Metaluminous
35
Igneous rock based on AlO concentration: Al2O3 < Na2O +K2O
Peralkaline
36
A very dark-colored rock, depleted in SiO 2 and commonly enriched in the minerals pyroxene, olivine, amphibole, and plagioclase. Ultramafic plutonic rocks occur in Earth’s Mantle
Peridotite
37
A fine-grained dark-colored (mafic), SiO 2- poor (Basic) rock rich in plagioclase, pyroxene, and olivine
Basalt
38
A coarse-grained dark-colored, silica-poor rock rich in plagioclase, pyroxene, and olivine
Gabbro
39
Fine-grained gray-colored to salt and pepper-colored rocks rich in hornblende, pyroxene, and plagioclase. Andesite and diorite contain more than half to almost two-thirds SiO 2.
Andesite
40
A coarse-grained gray-colored to salt and pepper-colored rocks rich in hornblende, pyroxene, and plagioclase. Andesite and diorite contain more than half to almost two-thirds SiO 2.
Diorite
41
A coarse-grained light-colored (felsic) rock, containing approximately two-thirds SiO2, rich in plagioclase, alkali feldspar, and quartz, and also contains small amounts of hornblende and biotite.
granodiorite
42
A fine-grained light-colored (felsic) rock, containing approximately two-thirds SiO2, rich in plagioclase, alkali feldspar, and quartz, and also contains small amounts of hornblende and biotite.
Dacite
43
A fine-grain light-colored (felsic) rock containing more than two-thirds SiO 2 (silicic or acidic) and rich in quartz, alkali feldspar with small percentages of plagioclase and biotite
Rhyolite
44
A coarse-grain light-colored (felsic) rock containing more than two-thirds SiO 2 (silicic or acidic) and rich in quartz, alkali feldspar with small percentages of plagioclase and biotite
Granite
45
light-colored non-crystalline vesicular rocks characterized by the absence of crystals.
pumice
46
dark-colored non-crystalline vesicular rocks characterized by the absence of crystals.
Scoria
47
non-crystalline rocks include those with glassy textures
Obsidian
48
Non-crystalline rocks that are enriched in rock pyroclastic fragments that are volcanic ash to gravel size.
Tuff
49
magma emplaced onto the surface of the Earth as coherent lava flows or as fragmental deposits. These rocks are typically aphanitic and glass
Extrusive (volcanic)
50
igneous rocks formed at depth; typically phaneritic
Intrusive (plutonic)
51
formed at intermediate depths not clearly distinct from those of volcanic and plutonic rocks. They can have fabric similar to that of plutonic and volcanic rocks.
hypabyssal rocks