Igneous Rocks Flashcards
The rate of cooling affects the texture
- Fast cooling: extrusive (at or near-surface)
- Slow cooling: intrusive (buried deeply), crystals are bigger b/c lots of time to grow
Texture in igneous rocks describes:
- Crystal size
- Porosity (pores)
- If it is made up of fragments of volcanic debris
Common igneous textures:
- Glassy (no crystals)
- Aphanitic (small crystals)
- Phaneritic (large crystals)
- Porphyritic (two crystal sizes = multistage cooling)
- Pyroclastic (fragments of rocks and crystals)
- Vesicular (holes/pores)
What is the composition of igneous rocks?
The composition of an igneous rock is inherited from the molten rock from which it formed
Felsic (lots of silica) mineral characteristics:
- Light in colour
- Iron and magnesium poor
Mafic mineral characteristics:
- Dark in colour
- Iron and magnesium-rich
The composition of the mantle is:
ultramafic
If magma and lava come from the mantle, why aren’t all igneous rocks ultramafic?
- The mantle partially melts, lowest melting temps melt first which are chemically distinct from the rest of the mantle
- The most silica-rich minerals are preferentially extracted and turned into magma (lowest melting temps!!)
Intermediate rocks contain more silica than mafic rocks. Can be produced through:
- Crystal settling in a mafic magma (crystals pull out Fe and Mg, creating silica-rich magma)
- Partial melting of a mafic rock
- Mixing mafic magma with felsic magma
- Assimilating felsic rocks into mafic magma
Producing felsic magma requires many phases of:
partial melting and/or crystal settling to increase silica content
Igneous Phaneritic Rocks
G.D.G
Granite, Diorite, Gabbro
Igneous Aphanitic Rocks
B.A.R
Basalt, Andesite, Rhyolite
Felsic Igneous Rocks
Rhyolite, Granite
Intermediate Igneous Rocks
Andesite, Diorite
Mafic Igneous Rocks
Basalt, Gabbro