metamorphic change (3)
Neo-crystallization
Foliation
Re-crystallization
Plastic deformation
mineral grains soften and deform
increased temperature and pressure
dont break, behave plastically
Agents of metamorphism (4)
1) Heat (T)
2) Pressure (P)
3) Compression and shear
4) Hot water
Sources of heat (3)
1) Geothermal gradient
2) Magmatic intrusions
3) Tectonic compression
Where does metamorphism occur?
2-12 Kbars = 6.5-40km
Kinds of differential stress (2)
Normal stress
Shear stress
Normal stress
operates perpendicular to surface
Tension-compression
Shear stress
moves one part of the material sideways
causes material to be smeared out
Shape changes due to differential stress (2)
Equant: equal in all dimensions
Inequant: not equal in all dimensions
Do metamorphic rocks prefer equant of inequant dimensions
Inequant dimensions
How does preferred mineral orientation develop?
Hydrothermal alteration is called _______
Metasomatism
Major divisions of Metamorphic rocks (2)
1) foliated
2) non-foliated
Foliated metamorphic rocks
Non-foliated metamorphic rocks
Foliation
Slate
Fine grained
low grade metamorphic shale
Schist
Fine to course rock with larger Mica’s
medium to high grade metamorphism
shistosity (type of foliation)
Large non-mica minerals
porphyroblasts
Gneiss
distinct banded foliation
light bands: Feldspar/quartz
dark bands: biotite/amphibole
compositional banding development (3)
1) Original layering in the protolith
2) Extensive high T shearing
3) Metamorphic differentiation
Migmatite
Partially melted gneiss
feature of igneous and metamorphic rock
Hornfels
alteration by heating (contact metamorphism)
baked contact by igneous rock
Amphibolite
protolith of gabbro or basalt
High is Mg and Fe
foliation under differential stress