Chap 14/15: Metamorphic rocks

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metamorphism definition

changes in minerology and texture in the (usually) solid state due to changing external conditions (Pressure and temperature) after 200C

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how are new minerals formed in metamorphism without melting

atoms are moved one by one along grain boundaries to form a new mineral

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diagenesis meaning

chemical, physical, and biological changes that affect sediment after initial deposition up to 200C (after 200C is metamorphism)

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melting temperature occurance

600-800C, bound after metamorphism where igneous processes typically lie

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protolith meaning

starting material for a rock ie parent rock

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order of metamorphic progression with increasing temperature and pressure

  • shale

  • slate

  • phyllite

  • schist

  • gneiss

  • migmatite (partially melted)

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what happens along the metamorphic progression

  • new or different minerals appear

  • folliation appears

  • increased grain size

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driving forces of metamorphism?

  • heat

  • pressure

  • fluids

  • deformation

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lithostatic pressure meaning

pressure induced from rocks

(at deep levels, pressure is equal due to flowing rock)

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hydrostatic pressure meaning

pressure induced from liquids

(pressure is equally distributed)

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typical geothermal gradient

15C/km

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regional metamorphism

metamorphism that occurs over a large scale

  • heat transfer occurs when rocks heat after thrusting on top of each other which causes lower rocks to heat

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contact metamorphism

metamorphism that occurs over small region

  • magma intrusion heats an area

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contact heat transfer is controlled by (3)

  • size of intrusion

  • temperature of magma

  • fluid circulation

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heat capacity

adding the same amount of heat and energy to different materials will lead to different increases in temperature

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aureole

region of metamorphism surrounding an intrusion

  • larger intrusion = larger aureole

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what affects the size of an aureole (5)

  • temperature difference btwn intrusion and host

  • composition of intrusion and host

  • speed of emplacement

  • fluid interactions (ground water and magmatic fluids)

  • shape of intrusion

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amount of water as metamorphic progress occurs?

weight precent of water decreases due to dehydration reactions

  • shale (12-15%) to gneiss (0-1%)

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regional deformation

rock texture will changed due to differential stress which produces folliation

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contact deformation

since the metamorphism is static, there’s no metamorphic stress and no foliation

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fabric definition

the combined effects of mineral reactions and deformation throughout the metamorphic event and the subsequent return of the rock to the terrestrial surface

  • foliation is a type

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crystal settling

early formed crystals piling up at the bottom of a magma chamber

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what structure does quartz form in rocks like quartzite in thin section

triple grain bonds

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can calcite foliate?

calcite cannot since it does not have a long axis

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undulous extinction

texture resulting from a deformed crystal which causes the extinction to be wavy and irregular

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when does the reduction of grain size occur

extreme deformity that occurs when lots of heat is applied (mylonites)

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what metamorphic rock form is most useful when wanting to know about the temperature and pressure of the area

regional shales/pelites (marine origin)

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what metamorphic rock form is most useful when wanting to know about the metabasic rock

basaltic rocks

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pelite definition

alumina-rich rock that is sensitive to the metamorphic conditions

can define the general increasing metamorphic grade trend

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if a rock is on the border of having either kyanite and silimanite but one has a higher Gibbs energy and the other is lower, which form is taken?

Form with the lower gibbs energy

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pelite prograde minerals in order (7)

  • chlorite

  • biotite

  • garnet

  • staurolite

  • kyanite

  • silimanite

  • k-feldspar

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prograde meaning

the grade changes in order from low to high temperature

  • more common since energy is more available

  • loss of volatiles occurs here

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metabasic rock prograde minerals in order (5)

  • chlorite

  • epidote

  • amphibole

  • garnet

  • pyroxene

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retrograde meaning

the grade changes in order from high to low temperature

  • needed stuff for the minerals to revert are gone such as H2O and CO2 during peak metamorphism

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what conditions make plagioclase more calcium rich?

increased temperature and pressure

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how is the kinetics of the rocks shown?

via texture

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metamorphic facies

metamorphic rocks that form under the same pressure and temperature but different protoliths

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minerals in amphibolite shale facies

quartz, biotite, muscovite, and garnet

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minerals in amphibolite limestone facies

calcite

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minerals in amphibolite basalt facies

amphibole, plagioclase, quartz

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isograds meaning

lines of constant metamorphic grade where new minerals are seen

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metamorphic zone naming

named after highest grade metamorphic mineral between the isograds

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metasomatism

fluids passing through rock that bring new elements to replace old ones, changes bulk composition of the rock

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porphyroblasts

crystal in metamorphic rock that is significantly larger than other minerals in the rock

garnet and staurolite are common

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metamorphic grade

loosely states intensity of metamorphism using the formation of minerals at each stage (ie slate, phyllite…)

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conditions needed to form greenschist

  • regional metamorphism

  • mid temp and pressure

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conditions needed to form blueschist

  • mid to high pressure

  • low temp

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conditions needed to form zeolite

  • low temp

  • low pressure

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conditions needed to form eclogite

  • high pressure

  • mid to high temp

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conditions needed to form hornfels

  • low pressure

  • mid to high temp

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conditions needed to form amphibolite

  • mid pressure

  • mid to high temp

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conditions needed to form granulite

  • mid to high pressure

  • high temperature

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geothermometer meaning

metamorphic reactions that are sensitive to temperature changes so can be used to determine metamorphic temperatures

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geobarometers

metamorphic reactions that are sensitive to pressure changes so can be used to determine metamorphic pressures but much less common

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skarns

calcsilicate rich rocks that can form Fe-ore deposits

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soapstone

mixture of serpentine and talc from the metamorphism of ultramafic igneous rocks

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index mineral

a mineral that forms in a metamorphized rock that indicates the minimum pressure and temperature in which the rock forms

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