Day 2 Correl Flashcards
A general term used for describing relative T and P conditions under which metamorphic rocks form
Metamorphic Grade
T and P conditions under low grade metamorphism
T: 200-400°C
P: 1-6 Kbars
T and P conditions under high grade metamorphism
T: 500-1000°C
P: 12-40 Kbars
Arrange in increasing metamorphism: phyllite, shale, slate, gneiss, schist
Shale, slate, phyllite, schist, gneiss
Minerals stable at lower T are only partially replaced by those stable at higher T
Prograde metamorphism
Incomplete replacement of minerals stable at high T by those stable at low T
Retrograde metamorphism
Set of rocks representing the full range of possible chemistries within a limited range of metamorphic conditions (Eskola, 1915)
Metamorphic facies
What rocks do Eskola used to base his naming of the facies?
Metabasic basic rocks
Facie containing the green minerals, chlorite
and actinolite, along with other minerals like plagioclase, biotite, and garnet.
Greenschist
Facie containing the blue sodic amphibole, glaucophane (along with garnet and lawsonite)
Blueschist
Facie containing
mostly hornblende and plagioclase
Amphibolite
Facie containing the green
sodic pyroxene called omphacite and garnet
Eclogite
Facies named after the textures of the rocks, with ______
being the rocks commonly found in contact metamorphic aureoles (high temperature,
low pressure environments)
Hornfels
Facies named after the textures of the rocks, with ______ being coarse grained rocks with a granulitic texture and being generally free of hydrous minerals
Granulites
Facies containing basic rocks containing zeolite minerals
Zeolite
High T and P facie
Eclogite
What is the geothermal gradient that would cause prograde metamorphism to
occur along a sequence of facies
10 C/km
Where does high pressure facies series would be expected to occur? (zeolite-blueschist-eclogite)
Areas near subduction zones where cool lithosphere is pushed to higher
pressure
A facie series that would produce a succession of facies from zeolite to prehnite pumpellyite to greenschist to amphibolite to granulite. Expected in areas undergoing an orogenic event.
Medium pressure series or Barrovian facies series
A slightly higher geothermal gradient would produce the same succession of facies (as Barrovian), but pelitic rocks would show a change in the Al2SiO5 minerals from kyanite to andalusite to sillimanite
Low pressure series or
Buchan facies series
A facie series along very high geothermal gradients, such as might be expected in the vicinity of intruding magmas
Contact facies series
To distinguish between the true geothermal gradient and that deduced from the facies series, the deduced geothermal gradient is called the
metamorphic field gradient
4 stages encountered by rocks as rocks are pushed deeper into the Earth as a result of tectonism
Burial, Heating, Uplift, Unroofing
Defined as a pervasive planar structure that results from the nearly parallel alignment of sheet silicate minerals and/or compositional and mineralogical layering in the rock.
Foliation