Petrology Flashcards
(44 cards)
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
b. plagioclase feldspar
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
d. alkali feldspar
SiO2 content of ultramafic mineral
a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %
c. <45 wt. %
SiO2 content of mafic mineral
a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %
d. 45 - 52 wt. %
SiO2 content of intermediate mineral
a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %
b. 52 - 66 wt. %
SiO2 content of felsic mineral
a. >66 wt. %
b. 52 - 66 wt. %
c. <45 wt. %
d. 45 - 52 wt. %
a. >66 wt. %
Igneous rocks with this texture usually occur from the rapid crystallization of lava.
a. aphanitic
b. pegmatitic
c. glassy
a. aphanitic
This texture forms when lava from a volcanic eruption cools very rapidly such that no crystallization occurs.
a. aphanitic
b. pegmatitic
c. glassy
c. glassy
This type of texture id formed when magma cools and some minerals increase in size extensively.
a. aphanitic
b. pegmatitic
c. glassy
b. pegmatitic
form when violent volcanic eruptions throw the lava into the atmosphere creating fragmental and glassy materials.
a. porphyritic
b. phaneritic
c. pyroclastic
c. pyroclastic
This texture is seen in plutonic igneous rocks, which underwent slow crystallization underneath the surface of the earth.
a. porphyritic
b. phaneritic
c. pyroclastic
b. phaneritic
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. porphyritic
Rocks composed mostly of pyroxene, calcium-rich plagioclase, and minor amounts of olivine.
a. ultramafic
b. mafic
c. intermediate
d. felsic
b. mafic
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. ultramafic
Rocks composed mostly of biotite, muscovite, sodium-rich plagioclase feldspars, potassium feldspars, and quartz
a. ultramafic
b. mafic
c. intermediate
d. felsic
d. felsic
Rocks composed mostly of hornblende and plagioclase feldspars
a. ultramafic
b. mafic
c. intermediate
d. felsic
c. intermediate
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
e. pillow basalt
Molten rock that flows out of a volcano during eruption
a. cinders
b. lava
c. pumice
d. tephra
e. pillow basalt
b. lava
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
d. tephra
A volcanic glass that is associated with violent volcanic eruptions.
a. cinders
b. lava
c. pumice
d. tephra
e. pillow basalt
c. pumice
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
a. cinders
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
b. burial metamorphism
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
d. ocean floor metamorphism
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. faultzone and impact metamorphism