Review Concepts on Deformation and Metamorphism. Which statement regarding synclines is true? A....

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Review Concepts on Deformation and Metamorphism

Which statement regarding synclines is true?

A. Limbs dip toward the axial plane where the oldest strata are exposed.B. Limbs dip toward the axial plane where the youngest strata are exposed.C. Limbs dip away from the axial plane where the oldest strata are exposed.D. Limbs dip away from the axial plane where the youngest strata are exposed.

Rock folding

Which statement regarding synclines is true?

A. Limbs dip toward the axial plane where the oldest strata are exposed.B. Limbs dip toward the axial plane where the youngest strata are exposed.C. Limbs dip away from the axial plane where the oldest strata are exposed.D. Limbs dip away from the axial plane where the youngest strata are exposed.

Rock folding

What characterizes a fold as being a plunging fold?

A. The limbs dip at different angles from one another.B. The limbs both dip in the same direction.C. The axial plane is not vertical.D. The fold axis is not horizontal.

Rock folding

What characterizes a fold as being a plunging fold?

A. The limbs dip at different angles from one another.B. The limbs both dip in the same direction.C. The axial plane is not vertical.D. The fold axis is not horizontal.

Rock folding

Faults

• Faults are classified by:A. Map patternB. Stress fieldC. AgeD. Dip and relative motion

Faults

• Faults are classified by:A. Map patternB. Stress fieldC. AgeD. Dip and relative motion

Faults

A normal Fault is characterized byA. Tensional StressB. Steep Dip (>45o)C. Hanging wall down relative to footwallD. All of the above

Faults

A normal Fault is characterized byA. Tensional StressB. Steep Dip (>45o)C. Hanging wall down relative to footwallD. All of the above

Depth,km

0

35

75

Asthenosphere

Continental crust

Continental crust

Regional metamorphism Oceanic

crust

Oceaniclithosphere

Shockmetamorphism

Regionalmetamorphism

Regionalhigh-pressuremetamorphism

Contactmetamorphism

Burialmetamorphism

Continental mantle lithosphere

Continental mantle lithosphere

Water

Seafloormetamorphism

Which kind of metamorphism is caused primarily by increasing temperature with little change in pressure?

A. Regional MetamorphismB. Contact metamorphismC. Burial MetamorphismD. Subduction-zone metamorphism

The lithosphere and asthenosphere interact to metamorphose rock

Which kind of metamorphism is caused primarily by increasing temperature with little change in pressure?

A. Regional MetamorphismB. Contact metamorphismC. Burial MetamorphismD. Subduction-zone metamorphism

The lithosphere and asthenosphere interact to metamorphose rock

High-pressure regional metamorphism is most closely associated with which tectonic environment?

A. Continental riftingB. Mid-ocean ridgeC. Subduction zoneD. Meteorite impact

The lithosphere and asthenosphere interact to metamorphose rock

High-pressure regional metamorphism is most closely associated with which tectonic environment?

A. Continental riftingB. Mid-ocean ridgeC. Subduction zoneD. Meteorite impact

The lithosphere and asthenosphere interact to metamorphose rock

Seafloor metamorphism that occurs at mid-ocean ridges is caused by:

A. Directed pressureB. Confining pressure C. MetasomatismD. All of the above

The lithosphere and asthenosphere interact to metamorphose rock

Seafloor metamorphism that occurs at mid-ocean ridges is caused by:

A. Directed pressureB. Confining pressure C. MetasomatismD. All of the above

The lithosphere and asthenosphere interact to metamorphose rock

Increasing intensity of metamorphism

Increasing crystal size

Increasing coarseness of foliation

Low grade Intermediate grade High grade

Slate Phyllite Schist(abundantmicaceousminerals)

Gneiss(fewer

micaceousminerals)

Migmatite

Slaty cleavage Schistosity Banding Banding

Diagenesis Low grade Intermediategrade

High grade

Canada

NY

VT

ME

NH

MA

CT

RI

Isograds

Key: Notmetamorphosed

Chlorite zone

Biotite zone

Garnet zone

Staurolite zone

Sillimanite zone

Lowgrade

Medium grade

High grade

Index minerals define metamorphic zones. Isograds can be

used to plot thedegree of metamorphism.

Degree of metamorphism

Diagenesis

Greenschists

Low Intermediate

Amphibolites Granulites

High

Chlorite

White mica (mainly muscovite)

Biotite

Garnet

Staurolite

Sillimanite

Kyanite

Albite (sodium plagioclase)

With increasing metamorphicgrade, mineral compositionchanges.

Mineral suites definemetamorphic facies.

How do crystal size and foliation change with increasing intensity of metamorphism?

A. Grain size increases and foliation becomes less coarse.B. Grain size decreases and foliation becomes coarser.C. Both grain size and foliation coarseness decrease.D. Both grain size and foliation coarseness increase.

Texture, index minerals, grade, and facies describe metamorphism

How do crystal size and foliation change with increasing intensity of metamorphism?

A. Grain size increases and foliation becomes less coarse.B. Grain size decreases and foliation becomes coarser.C. Both grain size and foliation coarseness decrease.D. Both grain size and foliation coarseness increase.

Texture, index minerals, grade, and facies describe metamorphism

Which list places foliation textures in order of increasing metamorphic grade (low grade to high grade)?

A. Slate, gneiss, phyllite, schistB. Slate, phyllite, schist, gneissC. Gneiss, schist, slate, phylliteD. Gneiss, phyllite, schist, slate

Texture, index minerals, grade, and facies describe metamorphism

Which list places foliation textures in order of increasing metamorphic grade (low grade to high grade)?

A. Slate, gneiss, phyllite, schistB. Slate, phyllite, schist, gneissC. Gneiss, schist, slate, phylliteD. Gneiss, phyllite, schist, slate

Texture, index minerals, grade, and facies describe metamorphism

Metamorphic facies are defined by:

A. Suites of mineralsB. Foliation texturesC. Pressures and temperaturesD. Tectonic environments

Texture, index minerals, grade, and facies describe metamorphism

Metamorphic facies are defined by:

A. Suites of mineralsB. Foliation texturesC. Pressures and temperaturesD. Tectonic environments

Texture, index minerals, grade, and facies describe metamorphism