Igneous Rocks Flashcards

1
Q

Igneous Rocks

A

Formed by minerals crystallising from a melt known as magma (or, when extruded at the Earth’s surface)
There are two types of igneous rock types, Intrusive/Plutonic and Extrusive/Volcanic.

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2
Q

Intrusive/Plutonic

A
  • Formed when magma solidifies deep underground.
  • Includes granites, the main rock of continents.
  • Intrusive/plutonic rocks cooled slowly deep within the Earth and are coarse-grained or phaneritic (most crystals > 1mm -bigger than 1mm)
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3
Q

Extrusive/Volcanic

A
  • Formed when magma solidifies at the Earth’s surface as lava
  • Includes basalts, the main rock in the ocean floor
  • Extrusive/volcanic rocks cooled quickly at or near Earth’s surface, giving crystals little time to grow. These rocks tend to be fine-grained or aphanitic (most crystals <1mm- smaller than 1mm)
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4
Q

Name/describe 2 igneous rock textures (of igneous rock)

A

-Phaneritic (coarse) Texture
Large Crystals
Magma cooled & crystallised slowly

-Aphanitic
Small Crystals
Magma cooled & crystallised more quickly

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5
Q

Extrusive rock examples

A

Volcanic (fine grained)

  • Rhyolite (Acid- >65% Sio2)
  • Andesite (Intermediate- 52-65% SiO2)
  • Basalt (Basic- 45-52% SiO2)
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6
Q

Intrusive rock examples

A

Hypabyssal (med. grained)

  • Porphyry (Acid- >65% SiO2)
  • Porphyrite (Intermediate- 52-65% SiO2)
  • Dolerite (Basic- 45-52% SiO2)

Plutonic (coarse grained)

  • Granite (Acid- >65% SiO2)
  • Diorite (Intermediate- 52-65% SiO2)
  • Gabbro (Basic- 45-52% SiO2)
  • Peridotite (Ultra Basic- <45% SiO2)
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7
Q

Sills and Dykes

A

(within the earth’s crust)
Sill- horizontal (or sub-horizontal) layer of solidified lava
Dyke- when injected vertically

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8
Q

Identification Summary (examples)

A
Light coloured (Acid):
Coarse texture = Granite 
Medium texture = Micro-granite 
Fine texture = Rhyolite 
Dark Colour (Basic):
Coarse texture = Gabbro
Medium texture = Dolerite 
Fine texture = Basalt
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9
Q

Felsic

A
  • Light coloured minerals (quartz, alkali feldspar, and some plagioclase feldspar)
  • Rich Si, Na, Al and K and poor in Fe and Mg
  • Dark coloured minerals biotite and amphibole are present, but only in minor amounts

Example- Granite

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10
Q

Intermediate

A

-Rocks contain roughly equal amounts of dark-coloured minerals and light-coloured minerals

Example- Andesite

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11
Q

Mafic

A
  • Abundant dark-coloured minerals (olivine, pyroxene, and plagioclase)
  • These are compositionally rich in Fe, Mg and Ca.

Example- Basalt

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12
Q

Ultramafic

A
  • Fe and Mg-rich minerals from the mantle (olivine and pyroxene, but not plagioclase).
  • Compositionally rich in Fe, Mg and Ca, but poor in Si

Example- Olivine

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