Igneous Textures Flashcards
Broad classification of igneous rocks based on the degree of crystallinity.
Igneous Textures
Fully developed crystals with clear faces, formed from slowly cooling magma.
Euhedral/ Idiomorphic
Partially complete crystal form
Subhedral
Crystals that lack any observable faces; fitting into available spaces between other crystals.
Anhedral/ Xenomorphic
A mix of euhedral, subhedral, and anhedral grains.
Hypidiomorphic-granular Texture
Wholly glassy texture
Holohyaline
Partially crystalline/ partially glass texture
Hypocrystalline
Wholly crystalline texture
Holocrystalline
contains small crystals less than 1 mm in diameter, and are associated with volcanic rocks that cool quickly on Earth’s Surface
Aphanitic
Igneous rocks with crystals so small that even a microscope can’t see them clearly.
Cryptocrystalline
Rocks with small crystals that are visible with a petrographic microscope.
Microcrystalline
Very small crystals that can’t be seen with the naked eye but can be identified using a petrographic microscope.
Microlites
large crystals averaging 1mm to 30mm
Phaneritic
1 mm - 3 mm
Fine-grained
3 mm - 10 mm
Medium-grained
10 mm - 30 mm
Coarse-grained
This texture has two different crystal sizes because the rock cooled in two stages.
Porphyritic
Phenocrysts forms in what size of crystal?
LARGE
What is fine-grained material in a porphyritic rock.
Groundmass
Type of porphyritic texture where all crystals are visible to the naked eye, with phenocrysts being larger than the surrounding groundmass.
Porphyritic-Phaneritic
Type of porphyritic texture where the phenocrysts are embedded in a groundmass that is too fine-grained to see clearly.
Porphyritic-Aphanitic
Large crystals averaging more than 30 mm in diameter, and develop most commonly in granitic plutons with high volatile contents.
Pegmatitic
What is an igneous rocks with pegmatitic texture?
Pegmatite
This measures how many new crystals form in a certain amount of space over a certain amount of time.
Crystal Nucleation Rate