an introduction to metamorphism and metamorphic rocks
TRANSCRIPT
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metamorphism and metamorphic rocks�
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the rock cycle�
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metamorphism • high enough temperature & pressure to “change” rocks�
"but not high enough to melt rocks�" "…changes to rocks occur in the solid-state…�
• hot, reactive fluids also contribute�
• old minerals, unstable under new P, T �"conditions, re-crystallize into �" "new minerals�
• metamorphism occurs at depth; cannot�"see metamorphic rocks unless�" "they are uplifted�
• new rocks are metamorphic rocks�
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Metamorphism: Fundamental Questions�
• What are the subsolidus changes in fabric and composition that occur during metamorphism?�
• What transfers mass and energy to cause these changes?�
• In what tectonic settings does metamorphism occur?�
• How does the study of metamorphic rocks and processes help us understand plate tectonics and Earth’s evolution?�
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Metamorphism: Simple Definitions �
• Metamorphism is defined as physical and chemical changes that occur in pre-existing rocks (igneous, metamorphic, or sedimentary) in the solid state that yield in a lower free energy state as a result of changes in conditions (e.g. T and P).�
– Prograde: Increasing T and P�– Retrograde: Decreasing T and P�
• Diagenesis occurs at relatively low T and P and grades into metamorphism.�
• Melting or migmatization occurs at the most intense, i.e. highest T an P limits of metamorphism and therefore grades into igneous processes.�
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General P/T Conditions of Metamorphism �
From Spear, 1993
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metamorphic rocks: controlling factors�• parent rock composition (also called protolith)�
• temperature and pressure during metamorphism�
• tectonic forces�
• fluids�
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no new material is added to rock during metamorphism�
if parent material contains only one mineral�
limestone
marble (CaCO3)�
limestone (CaCO3)�
parent rock composition�
metamorphic rock will have similar composition to parent rock�
resultant metamorphic rock will only have one mineral�"--mineral will be recrystallized (texture changes)--�
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limestone under microscope�(stained)�
(note fragments of shells) �
marble under microscope�(note interconnecting grains) �
texture changes�
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if parent material contains many minerals…�
garnet growing � garnet schist (metamorphic rock)�
…old minerals will recombine to form new minerals�
clay, quartz, mica, and volcanic fragments in a sandstone�"will combine to form new metamorphic minerals�
example is garnet: which grows during metamorphism�
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heat is essential�
temperature during metamorphism�
• heat from Earth’s deep interior�
• all minerals stable over finite temperature range�
• higher temperatures than range cause melting�" "(and therefore generates igneous rocks) �
think about mixing flour, yeast, water, salt….�
….nothing happens until they have a heat source�" " and then they make bread�
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pressure in the Earth acts the same in all directions�
pressure is proportional�to depth in the Earth�
look at example with deep water�
pressure increases�with depth �
volume decreases�with depth �
pressure during metamorphism�
Increases about 1 kilobar per 3.3 km�or 30 MPa/km (megapascals/km)�
high pressure minerals: more compact and dense�
--in rocks, grains pack together-- �
consequence on cube is squeezing �into smaller cube�
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tectonic forces - driven by plate motion!�lead to forces that are not equal in all directions (differential stress)�
compressive stress (hands squeeze together)�causes flattening at 90° to stress�
shearing (hands rubbing together) �causes flattening parallel to stress�
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fluids �• hot water (water vapor) most important�
• heat causes unstable minerals to release water�
• water reacts with surrounding rocks �"and transports dissolved material and ions�
time�• metamorphism may take millions of years�
• longer times allow new minerals to grow larger�"--coarser grained rocks �
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Controlling Factors in Metamorphism �Note that metamorphic�equilibration is also�strongly affected by�kinetic factors, which �are not illustrated.�
Four Factors:�1) Temperature�2) Pressure�3) Fluid activity �4) Deviatoric stress �
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metamorphic rocks: basic classification�
foliated (layered) �
non-foliated (non-layered) �
type of foliation -- e.g. slaty �
composition -- e.g. marble �
based on rock texture�
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flattened pebbles in metamorphic rock�
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foliation�
foliated (layered) metamorphic rocks�results from differential stress (not equal in all directions)�
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non-foliated � foliated�
appearance under microscope�
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foliated metamorphic rock: slate �
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foliated metamorphic rock: slate �
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foliated metamorphic rock: phyllite (higher T, P than slate)�
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garnet�
foliated metamorphic rock: schist (higher T, P than phyllite)�…new minerals grow -- garnet (large, roundish grains)�
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schist under microscope�
garnet �
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banding of quartz/feldspar and ferromagnesian minerals�
foliated metamorphic rock: gneiss (higher T, P than schist)�
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non-foliated (non-layered) metamorphic rocks�results from equal pressure (or stress) in all directions�
named on the basis of their composition �
limestone (CaCO3)� marble (CaCO3)�
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non-foliated metamorphic rocks: quartzite�
metamorphosed �quartz sandstone�
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Photo credit: R. Weller
non-foliated metamorphic rocks: hornfels�
metamorphosed �basalt�
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types of metamorphism�contact metamorphism�
• occurs adjacent to magma bodies intruding�"cooler country rock -- “contact”�
• produces non-foliated metamorphic rocks�• happens in a narrow zone of contact�
"(~1 to 100 m wide) known as aureole�• forms fine-grained (e.g. hornfels) or�
"coarse-grained (e.g. marble) rocks�
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types of metamorphism�regional metamorphism�
• occurs over wide region and � mostly in deformed�
"mountain ranges�• produces foliated metamorphic � rocks �
• happens at high pressures and� over a range of temperature�
• increases in pressures and� temperatures forms rocks of�
"higher metamorphic grade�
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other types of metamorphism (less common)�
• produces migmatites, which� have both intrusive and�
"metamorphic textures�
• occurs during impact events�
partial melting during metamorphism�
shock metamorphism�
• yields very high pressures�
• forms “shocked” rocks around� impact craters�
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Shock Metamorphism�• Related to impacts of objects on planetary
surfaces (asteroids and meteorites).�• Deformation (metamorphism) is extremely
rapid and transient.�• Achieve much higher peak metamorphic
temperatures and pressures than commonly observed in terrestrial environments.�
• Products include impact breccias, melts (tektites), and planer deformation features in quartz and feldspar.�
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Canyon Diablo Iron Meteorite
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Planetary Impact Structures
Apollo 11 Image: The Moon Galileo Image: Ganymede
From: http://neo.jpl.nasa.gov/neo.html
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Impact Simulation - Gravity Dominated Model
Simulation by: James Richardson and H. Jay Melosh, Univ. of Arizona
Comet Impact Body: 1.5 g/cc 6 x 3 km
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Shock Metamorphism P/T Conditions �
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PDS in Shocked Quartz�
From: http://www.impact-structures.com/
Planar Deformation Structures�
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migmatite�
igneous and metamorphic�textures�
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hydrothermal alteration along mid-ocean ridge�
cold sea water encounters hot basalt, forms steam, alters minerals�
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black smoker offshore Pacific Northwest�
hot steam/sea water cools as it emerges into ocean and�precipitates metals�
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temperatures cooler in down-going (subducting) plate�(dashed purple line is isotherm -- line of equal T)�
plate tectonics and metamorphism�regional metamorphism associated with convergent boundaries �
• pressure increases with depth�
• temperature varies laterally�
• different P, T conditions� yield different degrees�
"of metamorphism�