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How are metamorphic rocks produced
Created from parent rock (protolith) through increased temperature, pressure, and fluid volume.
Metamorphic Agents
heat,
pressure
hydrothermal fluids
Metamorphic textures
Foliated
Non-foliated
Foliated Rocks
created in areas undergoing regional metamorphism
Metamorphic GRADE
Low Grade-little heat and pressure
Low to Medium Grade- slight heat and pressure
Medium Grade- moderate heat and pressure
High Grade- high heat and pressure
Non-foliated rocks
Created in areas undergoing Contact metamorphism
Small scale-localized events, no directional stresses
OR when protolith is compositionally uniform
No alignment (e.g., marble, quartzite)
Slate
Foliated
LOW GRADE
From shale or mudstone
Phyllite
Foliated
Low to Medium grade
From Slate
Schist
Foliated
medium-high grade
Phyllite
Gneiss
Foliated
High grade
Schist, granite, shale
Hornfels
Non-foliated
No grade (contact metamorphism)
Shale
Quartzite
Non-foliated
medium-high grade
Sandstone
Marble
Non-foliated
Medium-high grade
Limestone or dolostone
Serpentinite
Usually non-foliated
Low grade
Peridotite
Anthracite Coal
Non-foliated
High grade
Bituminous coal
What is a fault?
break in rocks where movement/displacement has occurred
Types of faults
Normal fault
Reverse/Thrust fault
Strike Slip fault
Oblique Slip Fault
Normal Fault
hanging wall moves down relative to foot wall
Extensional environment
Reverse/Thrust fault
hanging wall moves up relative to foot wall
Compressional environment
Strike Slip fault
No vertical motion, only lateral
Left and right
Oblique Slip fault
both vertical and horizontal motion
What is a fold?
bends in a rock where forces have been applied over long periods of time
Types of folds
Syncline
Anticline
Basin
Dome
Syncline fold
U shaped
youngest rocks in the center
Anticline fold
ā© shaped
oldest rock in the center
Basin fold
360 syncline
youngest rock in the center
Dome fold
360 anticline
oldest rocks in the center