Final Chapter 3 Flashcards

1
Q

What are the eight common minerals that form igneous rocks? Which four are mafic (black or dark green),
and which four are felsic?

A

Mafic: Olivine, Amphibole, Pyroxene, biotite
Felsic: Na-rich plagioclase, quartz, k-feldspar, muscovite

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2
Q

According to Bowen’s reaction series, which three minerals tend to dominate mafic rocks, and which one of these minerals is not a mafic mineral? (‘Mafic’ means rich in Mg and/or Fe.)

A

-olivine, pyroxene, and ca-rich plagioclase feldspar
-plagioclase feldspar is not mafic

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3
Q

Which four minerals tend to occur in intermediate rocks?

A

feldspars, minor quartz, hornblende, and biotite

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4
Q

Which six minerals tend to occur in felsic rocks?

A

k-feldspar, na-plagioclase, quartz, and slight muscovite, biotite, amphibole

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5
Q

Which textures indicate intrusive rocks and which extrusive? Which indicate a two-stage cooling history?

A
  • coarse-grained textures indicate intrusive rocks
  • fine-grained texture indicate extrusive rocks
  • porphyritic textures indicate a two-stage cooling
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6
Q

Which of the following rocks form from lava flows and which are pyroclastic: Basalt, andesite, rhyolite, scoria, tuff, obsidian, pumice?

A

Lava flows: scoria, obsidian, and pumice
Pyroclastic: rhyolite, basalt, tuff, and andesite

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7
Q

Is obsidian glassy because it cools much faster than other lava flows? Explain.

A

yes, a glassy texture suggests rapid cooling that’s so quick that crystals did not have the time to grow

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8
Q

Are pegmatites extra coarse-grained because they cool much slower than other intrusive rocks? Explain.

A

pegmatites cool slowly and have extra water in the magma; the water promotes rapid crystal growth by speeding migration of chemical elements to the growing crystals

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9
Q

Along which types of plate boundaries do igneous rocks form?

A

igneous rocks form at convergent and divergent plate boundaries

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10
Q

What causes the partial melting that occurs along subduction zones? What causes the partial melting that
occurs along ocean ridges and continental rifts?

A

-partial melting from subduction zones is caused by the subducting plate releasing its water-rich fluids into the rocks of the overlying mantle
–partial melting from ocean ridges and continental rifts is caused by magma rising up the mantle and reaching a pressure decrease until eventually the hot peridotite partially melts

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11
Q

As part of the lab exercises you graphed the compositional trends formed by mafic to felsic rocks. Did this
trends suggest a continuum of rock compositions, or do igneous rocks naturally fall in to discrete and separate
compositions, with no intermediates?

A

???????

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