Crustal Deformation

      Why should we study the deformation of the crust…what can it tell us?

      What causes the crust to deform?

      How do we know when we are looking at deformed crust?

            Evidence for deformation

                  Folded rock

                  Faulted rock

                  Submerged or uplifted shorelines

                  Marine fossils on mountain tops

                  Deformed crystals

 

What causes rocks deform?

      Force = Stress

      Types of Stress

            Differential stress:  unequal stress in different directions

                  Compression, tension and shear

      Strain: how the rock reacts to stress

            Accumulation of energy in rock due to force

            Causes deformation

How do rocks deform?

      Plastic deformation

            Fold or flow

      Brittle deformation

            Break…i.e. faulting

 

Factors that control deformation

      Amount of stress

      Temperature

      Rock Composition

            Limestone? Sandstone?  Shale?

            All behave differently

      Strain Rate

            How much deformation with time

      Confining pressure

            High:  increases strength of rock

            Low:  decreases strength of rock

 

Deformation follows a path

      Elastic deformation

            Primary creep

            Remove stress rock returns to original shape

      Plastic deformation

            Secondary creep

            Slow strain rate; rock folds/flows--non-recoverable

      Brittle deformation

            Tertiary Creep

            Accelerated strain rate…rock fails

 

Folded structures

      Compressional stress

            Anticlines & synclines

            Plunging anticlines and synclines

      Domes: tensional stress

      Basins: compressional stress

 

Faults

      Represents Brittle deformation

      Crust that has broken

      Strain exceeds strength of rock

      2 groups of faults

            Gravity faults

            Shear faulting

 

How do faults and folds relate to mountain building and plate tectonics?

     

Mountain Building and the Evolution of the continents

Vocabulary to know:

      Orogenesis

            Mountain building

      Orogeny

            a singe episode of mountain building

      Craton or Shield

            The oldest and central portion of the continents

 

What are Mountains?

      Folded or faulted crust

      Continental Volcanics (more in a bit)

 

Mountains have “roots”

      2/3 of a mountain is “pushing” in to the mantle

      Similar to iceberg in water

      How do we know this?

            Discovered using gravity

 

All mass exerts a gravitational force on all other mass

The bigger the mass the greater the force

Mountains have a high gravitational anomaly and thin parts of the crust will have a low anomaly.

 

Gravitational Anomalies

      Unequal variations in gravity due to changes in mass

      Positive anomalies  

            High gravitational readings

            Caused by high amounts of mass

      What causes Positive anomalies?

            Plate collisions

                  Causes crust to thicken

            Volcanoes

                  Adds mass through lava

            Ice sheets

            Thick sedimentation

 

      Negative anomalies

            Low gravitational readings

            created by less mass

                  Sudden removal of surface mass (ice sheet)

                  Impact crater

 

Gravitational studies in 1700 & 1800’s discovered the roots of mountains

      Gravitational mapping across mountain regions expected a high gravitational reading due to large amounts of mass

      Smaller reading than expected

      Suggested that denser mantle material is displaced by less dense crust pushing down into the mantle creating the lower than        expected reading.

 

What does this imply?

 

1) Mountains have deep roots based on the gravity readings.

2) Mountains are a low density rock and float on surrounding denser mantle rocks

3) ~10% of mass is above mantle at anytime

            Most of a mountain are roots that we don’t see

Principle of Isostasy

      Isostosy of mountains:

            An equilibrium of the lithosphere with the asthenosphere.

            Mountains are crust floating in a gravitational balance

            Affects erosional behavior of mountains

 

 

Isostatic adjustment:  The process of establishing a new equilibrium as tectonic and earth processes disrupt equilibrium

 

How do mountains form?

      Primarily through plate interaction

            Subduction

            Collision

            Faulting

                  Normal

                  Thrust

                  reverse

            Folding

 

Passive continental margins

      Trailing edge of a continent (east coast of N. America)

      No mountain building or volcanism

      Erosion dominates

Active Continental Margins

      Leading Edge of a continent

      Convergent boundary

            Examples?

 

Why are Passive Margins important to the process of mountain building?

      Don’t always stay passive

      Collect sediments that will later become part of the continent when collision occurs

      Adds Mass

Continental to oceanic collisions

      Volcanism and plutonic activity

      Accretionary wedges

            Often become core and root of new mountains due to thrust faulting and folding

            Can melt and create plutons

            Can uplift, fold and create a parallel range of mountains

 

Terrane accretion

      Adding micro-continents onto continental margins

      2 types:

            Short distance travel

                  Transform faults

                        Baja and west side of San Andreas

                  Seafloor or near shore islands

            Long distance travel (>3000 miles)

                  Exotic terranes or suspect terranes

                  How do we ID them?

 

How to ID exotic terranes

      Abrupt changes

            in stratigraphy

            in fossils (types and ages)

            Paleo magnitism

            Age of rocks

      Often broken into segments

      Elongated and spread out

West Coast of N. America Created this way

 

Continental to Oceanic collisions can Eventually can lead to:

      Continental to Continental collisions

            Mountain building through compression and faulting

            Thickens ocean sediment on continental shelf

            Creates largest mountain ranges

            Lots of metamorphism

            Creates lots of faults (What type?)

 

Mountains that form away from plate boundaries.

      How would this occur?

            Structures?

 

Basin and Range

      Horsts and Grabens

            Create by a series of normal faults.

 

Major orogenies in N. America

      Trans-Hudson

      Wopmay

      Grenville

      Taconic

      Caladonian

      Acadian

      Antler

      Sonoma

      Nevadan

      Sevier

      Larimide