Kinds of metamorphism Lecture based on http://csmres.jmu.edu/geollab/Fichter/MetaRx/MetaKind.html And PowerPoint lecture of Dr. J.D. Winter http://www.whitman.edu/geology/winter/

The Types of Metamorphism Different approaches to classification 1. Based on principal process or agent Dynamic Metamorphism Thermal Metamorphism Dynamo-thermal Metamorphism

2. Based on setting (P-T conditions/tectonic) Contact Metamorphism Pyrometamorphism Regional Metamorphism Orogenic Metamorphism Burial Metamorphism Ocean Floor Metamorphism Hydrothermal Metamorphism Fault-Zone Metamorphism (cataclastic or mylonitic in your text) Impact or Shock Metamorphism

Types of metamorphism based on pressure and temperature conditions http://csmres.jmu.edu/geollab/Fichter/MetaRx/MetaKind.html

Blueschist metamorphism Geothermal gradient: Indicates the average increase of temperature with depth HIGH pressure/Low temperature Typically associated with subduction zones Example: Blueschist (from glaucophane)

Glaucophane in a blueschist (ppl). 1mm Glaucophane in a blueschist (ppl). http://www.union.edu/PUBLIC/GEODEPT/COURSES/petrology/met_minerals.htm#Amphiboles

Eclogite metamorphism VERY HIGH pressure/moderate temperature Happens in the mantle Example: Eclogite (pyroxene/garnet)

Eclogite (xpl) Eclogite (ppl)

Hydrothermal metamorphism Low pressure/low temperature Hot, chemically active waters react with the surrounding rocks Example: Serpentinite, soapstone

Hydrothermal metamorphism Usually involves METASOMATISM (metamorphism plus exchange of ions from an external source) Difficult type to constrain: hydrothermal effects often play some role in most of the other types of metamorphism

Contact metamorphism Low pressure/HIGH temperature “Country” rocks baked by igneous intrusion (pluton) Example: Hornfels, skarn (baked carbonate rocks), quartzite, marble

Contact Metamorphism Most easily recognized where a pluton is introduced into shallow rocks in a static environment (Pluton=intrusive igneous body, like a batholith) ® Hornfelses (granofelses) commonly with relict textures and structures

Spotted hornfels http://www.geolab.unc.edu/Petunia/IgMetAtlas/meta-micro/spottedhornfels.X.html

Pyrometamorphism A minor type of contact metamorphism Very high temperatures at very low pressures, generated by a volcanic or subvolcanic body Also developed in xenoliths (pieces of solid rocks carried up by magma) Pyrometamorphism may be accompanied by various degrees of partial melting

Barrovian metamorphism Also referred to as “regional” metamorphism Intermediate pressure/Low-high temperature Example: Slate-phyllite-schist-gneiss, also quartzite and marble

Regional Metamorphism sensu lato: metamorphism that affects a large body of rock, and thus covers a great lateral extent Three principal types: Orogenic metamorphism Burial metamorphism Ocean-floor metamorphism The term, “regional metamorphism” is often used synonymously with “orogenic metamorphism” (OROGENY=mountain building)

Orogenic Metamorphism is the type of metamorphism associated with convergent plate margins Dynamo-thermal: one or more episodes of orogeny with combined elevated geothermal gradients and deformation (differential stress) Foliated rocks are a characteristic product

Quartz-muscovite schist (xpl) Foliation Slate (ppl) Phyllite (xpl) Quartz Muscovite Quartz-muscovite schist (xpl) http://www.geolab.unc.edu/Petunia/IgMetAtlas/meta-micro/metamicro.html

Crenulation cleavage in a muscovite-biotite-garnet schist (xpl) http://www.geolab.unc.edu/Petunia/IgMetAtlas/meta-micro/metamicro.html

Gneiss under a microscope (xpl) Biotite Feldspar Quartz Gneiss in hand specimen http://www.geolab.unc.edu/Petunia/IgMetAtlas/meta-micro/metamicro.html

Calcite (note cleavage) Marble (xpl)

Burial metamorphism = low-grade metamorphism in sedimentary basins Metamorphic effects attributed to increased temperature and pressure due to burial Occurs in areas that have not experienced significant deformation or orogeny Mild deformation, no igneous intrusions discovered

Restricted to large, relatively undisturbed sedimentary piles away from active plate margins Term coined by Coombs (1961) based on Southland Syncline in New Zealand: thick pile (> 10 km) of Mesozoic volcaniclastics Modern examples: The Gulf of Mexico? Bengal Fan?

Ocean-Floor Metamorphism affects the oceanic crust at ocean ridge spreading centers A wide range of temperatures at relatively low pressure Seawater penetrates down fracture systems, where it becomes heated, and leaches metals and silica from the hot basalts Considerable metasomatic alteration, notably loss of Ca and Si and gain of Mg and Na

Highly altered chlorite-quartz rocks- distinctive high-Mg, low-Ca composition Black smokers - Another example of hydrothermal metamorphism

Fault-Zone and Impact Metamorphism High rates of deformation and strain with only minor recrystallization (a) Shallow fault zone with fault breccia (b) Slightly deeper fault zone (exposed by erosion) with some ductile flow and fault mylonite

Width of view=4mm

Fault-Zone and Impact Metamorphism High rates of deformation and strain with only minor recrystallization Impact metamorphism at meteorite (or other bolide) impact craters Both correlate with dynamic metamorphism, based on process