Petrology Flashcards

(44 cards)

1
Q

It is the most abundant mineral in the earth’s crust compromising 39% of earth’s crust

a. clay
b. plagioclase feldspar
c. pyroxene
d. quartz

A

b. plagioclase feldspar

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2
Q

It is one of the most abundant mineral in the earth’s crust compromising 12% of earth’s crust

a. nonsilicates
b. mica
c. amphibole
d. alkali feldspar

A

d. alkali feldspar

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3
Q

SiO2 content of ultramafic mineral

a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %

A

c. <45 wt. %

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4
Q

SiO2 content of mafic mineral

a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %

A

d. 45 - 52 wt. %

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5
Q

SiO2 content of intermediate mineral

a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %

A

b. 52 - 66 wt. %

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6
Q

SiO2 content of felsic mineral

a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %

A

a. >66 wt. %

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7
Q

Igneous rocks with this texture usually occur from the rapid crystallization of lava.

a. aphanitic
b. pegmatitic
c. glassy

A

a. aphanitic

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8
Q

This texture forms when lava from a volcanic eruption cools very rapidly such that no crystallization occurs.

a. aphanitic
b. pegmatitic
c. glassy

A

c. glassy

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9
Q

This type of texture id formed when magma cools and some minerals increase in size extensively.

a. aphanitic
b. pegmatitic
c. glassy

A

b. pegmatitic

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10
Q

form when violent volcanic eruptions throw the lava into the atmosphere creating fragmental and glassy materials.

a. porphyritic
b. phaneritic
c. pyroclastic

A

c. pyroclastic

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11
Q

This texture is seen in plutonic igneous rocks, which underwent slow crystallization underneath the surface of the earth.

a. porphyritic
b. phaneritic
c. pyroclastic

A

b. phaneritic

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12
Q

This texture is caused by the rapid change of conditions as the magma continues to cool down. The minerals that had been created earlier, by the slow cooling magma, will posses’ large crystals.

a. porphyritic
b. phaneritic
c. pyroclastic

A

a. porphyritic

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13
Q

Rocks composed mostly of pyroxene, calcium-rich plagioclase, and minor amounts of olivine.

a. ultramafic
b. mafic
c. intermediate
d. felsic

A

b. mafic

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14
Q

Their low silica and gas contents make them very fluid; i.e., they have a low viscosity, or resistance to flow

a. ultramafic
b. mafic
c. intermediate
d. felsic

A

a. ultramafic

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15
Q

Rocks composed mostly of biotite, muscovite, sodium-rich plagioclase feldspars, potassium feldspars, and quartz

a. ultramafic
b. mafic
c. intermediate
d. felsic

A

d. felsic

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16
Q

Rocks composed mostly of hornblende and plagioclase feldspars

a. ultramafic
b. mafic
c. intermediate
d. felsic

A

c. intermediate

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17
Q

Formed at spreading ridges on the ocean floor when two oceanic plates are separating

a. cinders
b. lava
c. pumice
d. tephra
e. pillow basalt

A

e. pillow basalt

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18
Q

Molten rock that flows out of a volcano during eruption

a. cinders
b. lava
c. pumice
d. tephra
e. pillow basalt

19
Q

Igneous rocks that have been airborne for a period of time before settling to the earth

a. cinders
b. lava
c. pumice
d. tephra
e. pillow basalt

20
Q

A volcanic glass that is associated with violent volcanic eruptions.

a. cinders
b. lava
c. pumice
d. tephra
e. pillow basalt

21
Q

Similar to pumice but usually made of iron-rich minerals found in basalt lava.

a. cinders
b. lava
c. pumice
d. tephra
e. pillow basalt

22
Q

P increases due to the weight of the overburden and T also increases due to the geothermal gradient.

a. faultzone and impact metamorphism
b. burial metamorphism
c. regional metamorphism
d. ocean floor metamorphism

A

b. burial metamorphism

23
Q

Interaction of heated seawater with newly-created oceanic crust at mid-ocean ridges.

a. faultzone and impact metamorphism
b. burial metamorphism
c. regional metamorphism
d. ocean floor metamorphism

A

d. ocean floor metamorphism

24
Q

Rock in the deep portions of faults undergoes dynamic metamorphism and creates a fine grained metamorphic rock called a mylonite.

a. faultzone and impact metamorphism
b. burial metamorphism
c. orogenic metamorphism
d. ocean floor metamorphism

A

a. faultzone and impact metamorphism

25
occurs during the development of island arcs, continental arcs, and continental collision zones. It is a dynamo-thermal type of metamorphism. a. faultzone and impact metamorphism b. burial metamorphism c. orogenic metamorphism d. ocean floor metamorphism
c. orogenic metamorphism
26
rocks undergo metamorphic reactions due to heating (little or no pressure change). when a hot igneous intrusion (magma) comes into contact with cold country rock, it creates a metamorphic aureole a. hydrothermal metamorphism b. contact metamorphism c. regional metamorphism
b. contact metamorphism
27
Characterized by involvement of hot aqueous fluid which passes through the metamorphosing rock that leads to changes in its chemical composition a. hydrothermal metamorphism b. contact metamorphism c. regional metamorphism
a. hydrothermal metamorphism
28
Complex composition, many different kinds of minerals. Has many new minerals produced with a change in T/P a. texture b. foliated c. equant mineral d. non-foliated
b. foliated
29
Simple composition with no new minerals form with a change in T/P a. texture b. foliated c. equant mineral d. non-foliated
d. non-foliated
30
Started out originally with clay minerals and as a result of metamorphism, alumna-rich minerals form. a. calcareous b. mafic c. pelitic d. quartzo-feldspathic
c. pelitic
31
Minerals like biotite, hornblende and plagioclase form during metamorphism and commonly produce amphibolites. a. calcareous b. mafic c. pelitic d. quartzo-feldspathic
b. mafic
32
Usually derived from limestones or dolostones, and thus contain an abundance of Calcite a. calcareous b. mafic c. pelitic d. quartzo-feldspathic
a. calcareous
33
Protoliths are usually granites, rhyolites, or arkose sandstone and metamorphism results in gneisses a. calcareous b. mafic c. pelitic d. quartzo-feldspathic
d. quartzo-feldspathic
34
Preferred orientation of these sheet silicates causes the rock to easily break along the planes parallel to the sheet silicates a. schist b. phyllite c. slate d. pophyroblasts
c. slate
35
The rock developed a near planar foliation caused by the preferred orientation of sheet silicates a. schist b. phyllite c. slate d. pophyroblasts
a. schist
36
The clay minerals have recrystallized into tiny micas which reflect a glossy luster. a. schist b. phyllite c. slate d. pophyroblasts
b. phyllite
37
When non-mica minerals (quartz, feldspars, kyanite, garnet, staurolite, and sillimanite) occur with a grain size greater than the rest of the rock, they are called _________. a. schist b. phyllite c. slate d. pophyroblasts
d. pophyroblasts
38
These dark colored minerals tend to become segregated in distinct bands through the rock, giving the rock a __________. a. migmatites b. granulite c. gneissic banding d. gneiss
c. gneissic banding
39
If the temperature reaches the solidus temperature, the rock may begin to melt and start to co-mingle with the solids. a. migmatites b. granulite c. gneissic banding d. gneiss
a. migmatites
40
At the highest grades of metamorphism, all of the hydrous minerals and sheet silicates become unstable and thus there are few minerals present that would show a preferred orientation resulting a ___________. a. migmatites b. granulite c. gneissic banding d. gneiss
b. granulite
41
As metamorphic grade increases, the sheet silicates become unstable and dark colored minerals like hornblende and pyroxene start to grow. a. migmatites b. granulite c. gneissic banding d. gneiss
d. gneiss
42
limestone or dolostone made up only if calcite or dolomite will metamorphose to a _______. a. amphibolite b. hornfels c. quartzite d. marble
d. marble
43
Very fine- grained rocks that usually form as a result from magma intruding into fine grained igneous rocks or shales a. amphibolite b. hornfels c. quartzite d. marble
b. hornfels
44
Dark-colored rocks with amphibole as their major mineral. a. amphibolite b. hornfels c. quartzite d. marble
a. amphibolite