EXAM 3 MATERIAL Flashcards
(180 cards)
describe hypabyssal rocks and what they are.
- form near the surface
- cool relatively quickly
- fine grained
describe plutonic rocks and what they are.
- form at depth
- cool slowly
- coarse grained/visible crystals
why do magmas form?
they form when rock is melted
why do magmas ascend upwards?
they are less dense than the surrounding country rock
how is modal rock analysis used?
used for the IUGS classification of igneous rocks
what is mineralological classification?
classifying rocks based on they mineralogical composition
what is the chemical composition classsification?
classifying rocks based on their chemical composition
describe the difficulty of obtaining modal analysis from the different rock types
- coarse-grained plutonic is easy
- fine-grained volcanic is difficult
- glassy rocks is impossible
how are igneous rocks classified?
- mode of occurrence
- mineralogical makeup
- chemical composition
what is the problem with historic classification?
contains a huge number of rock names, not used consistently
what method is used to classify very fine-grained/glassy rocks?
chemical analysis
what is latent heat of fusion?
the amount of energy that must be applied to a rock to melt it.
what role does latent heat of fusion play in melting?
prevents large scale melting in the earth
what are discordant intrusive magma bodies?
if the intrusive body cuts through the surrounding rock, it is discordant
what are Cordant intrusive magma bodies
if the intrusive body parallels the surrounding rock, it is Concordant
in what direction do magmas always intrude?
the minimum stress direction
what are dikes?
a vertical intrusive igenous body
what are sills?
a horizontal intrusive igneous body
what types of igneous intrusions are associated with crustal extension?
dikes and flood basalts
what types of igneous intrusions are associated with crustal compression?
plutons, sills
are intrusive dikes common at any of the plate boundaries?
YES
what are chilled margins?
edges of an igneous intrusion where magma cool rapidly due to contact with colder surrounding rock
how do chilled margins form?
magma cools rapidly due to contact with colder surrounding rock
what are cone sheets?
when pressure increases fractures propagate from the top of the magma chamber to the surface magma seeps in, creating cone sheets