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Figure 3.12
Igneous Rocks
(Lab )
The Rock
Cycle
Sedimentary Rocks
Metamorphic Rocks
(Lab )
(Lab )
Areas of
regional
metamorphism
Compressive
Stress
Compressive
Stress
Products of Regional Metamorphism
Products of Contact Metamorphism
Foliated texture forms
during compression
Non-foliated texture forms
during static pressure
Texture
Minerals
Other Diagnostic Metamorphic
Features
Rock Name
Protolith
Non-foliated
calcite, dolomite
cleavage faces of
calcite usually visible
Marble
Limestone
quartz
quartz grains are
intergrown
Quartzite
Quartz Sandstone
clay
looks like shale but
breaks into layers
Slate
Shale
muscovite, biotite
very fine-grained, but
has a sheen like satin
Phyllite
Shale
muscovite, biotite,
may have garnet
minerals are large
enough to see easily,
muscovite and biotite
grains are parallel to
each other
Schist
Shale
feldspar, biotite,
muscovite, quartz,
garnet
has layers of different
minerals
Gneiss
Any protolith
amphibole
layered black
amphibole grains
Amphibolite
Basalt or Andesite
Foliated
Texture
Minerals
Other Diagnostic Metamorphic
Features
Rock Name
Protolith
Non-foliated
calcite, dolomite
cleavage faces of
calcite usually visible
Marble
Limestone
quartz
quartz grains are
intergrown
Quartzite
Quartz Sandstone
clay
looks like shale but
breaks into layers
Slate
Shale
muscovite, biotite
very fine-grained, but
has a sheen like satin
Phyllite
Shale
muscovite, biotite,
may have garnet
minerals are large
enough to see easily,
muscovite and biotite
grains are parallel to
each other
Schist
Shale
feldspar, biotite,
muscovite, quartz,
garnet
has layers of different
minerals
Gneiss
Any protolith
amphibole
layered black
amphibole grains
Amphibolite
Basalt or Andesite
Foliated
 Identification of Metamorphic Rocks
 12 samples
 7 are metamorphic
 5 are igneous or sedimentary
 Protoliths and Geologic History
 For 2 of the metamorphic rocks:
 Match the metamorphic rock to its protolith (both from Part
One)
 Write a short geologic history of the sample
Formation of the protolith
2. Burial to the depth where metamorphism takes place
3. Metamorphism
4. Uplift and erosion to bring the metamorphic rocks to the
surface
1.
Metamorphic
Sample
Number
2
Metamorphic Rock
Name
Gneiss
Protolith
Sample
Number
Protolith Rock Name
7
Granite
Geologic History
1. Granitic magma
intruded in the Earth's
crust and crystallized to
form granite.
2. Granite was forced
deeper in the crust by
plate tectonics.
3. Granite was
metamorphosed to form
gneiss.
4. The rocks above the
gneiss were eroded away
to expose the gneiss at the
surface.
 Interpretation of Metamorphic Rocks
 Contact Metamorphism
 Match the protolith to the metamorphic rock
 Determine the thermal gradient (direction of increasing
temperature) during contact metamorphism
 Regional Metamorphism
 Using five metamorphic rocks (from Part One), determine
the direction of the thermal gradient during regional
metamorphism for this example
 Also, determine the direction of compressive stress during
metamorphism