Metamorphic + Time

34 flashcardsby Gretchen
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1
Metamorphic rocks
form when pre-existing rocks are exposed to increased pressure and/or temperature, causing solid-state recrystallization
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Protolith
the rock before
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Heat and pressure
Causes of Metamorphism (2)
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Recrystallization
Phase change
Neocrystallization
Pressure solution
Plastic deformation
Consequences of Metamorphism (5)
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Recrystallization
same mineral, new size and shape
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Phase change
same composition, new mineral
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Neocrystallization
growth of new mineral (chem and structure)
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Pressure solution
minerals smooshed together. Dissolution occurs at grain to grain contacts and new growth occurs in locations with less pressure
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Plastic deformation
changing shape without breaking under high pressure and temperature
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Porphyroblast
large crystal that grows within a finer-grained matrix during metamorphism
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Compression
squeezing a material
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Shear
moving part of a material sideways relative to another
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Dynamic (Regional) metamorphism
metamorphism with high pressure but relative low temperature that happens in subduction zones; happens over a large region
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Contact metamorphism
metamorphism where heat is transferred from melt to surrounding rock
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Burial metamorphism
metamorphism where, with depth, both pressure and temperature increase (but not extreme)
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Shock metamorphism
metamorphism with intense heat and pressure from shock wave pulse
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Foliation
planar rock fabric
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Uniformitarianism
the present is the key to the past
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Superposition
youngest on top
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Original horizontality
sediment layers are fairly horizontal when deposited and can be altered by deformation
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Lateral continuity
sediment generally deposited in continuous sheets. If later cut, you can assume once continuous
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Cross-cutting relationships
igneous intrusive must be younger than the rock it cuts across
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Baked contacts
heat transferred from igneous melt to surrounding rock. Evidence that surrounding rock existed prior to igneous rock
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Law of Inclusions
rock containing inclusion is younger than the inclusion
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Faunal succession
fossils that can be used for relative dating
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William “Strata” Smith
who realized that strata occurred in a predictable pattern and he could use fossils to trace rock layers. Made the first detailed nationwide geological map
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Angular unconformity
beds tilted and eroded prior to deposition of new horizontal bed on top. Forms between two strata not parallel to each other
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Radioactive decay
process by which the nucleus of an unstable atom loses energy by emitting radiation
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Nonconformity
igneous or metamorphic rock surface eroded and then sedimentary rock deposited on top. Forms between older metamorphic or igneous rocks and younger sediment strata deposited on top of them
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Disconformity
erosional surface between sedimentary rock layers where the older rock layer has been eroded but not tilted
Forms between parallel strata
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Electrons
Nuclear particles
Smaller nucleus
Electromagnetic radiation
Radiation can be one or more of the following (4)
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Isotope
same element (number of protons) but different number of neutrons
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Half-life
time required for one-half of parent to be converted into daughter
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Eon - Era - Period - Epoch - Age - Chron
Hierarchy of Geological Time
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