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Stratigraphy Principles of Stratigraphy Types of Stratigraphy Contacts Unconformities

Stratigraphy

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Stratigraphy

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Page 1: Stratigraphy

Stratigraphy

• Principles of Stratigraphy

• Types of Stratigraphy

• Contacts

• Unconformities

Page 2: Stratigraphy

Stratigraphy

“Stratigraphy can be defined as the complete triumph of terminology over facts and common sense.”

Attributed to P.D. Krynine by J. Ferm in Burton et al., 1987.

Page 3: Stratigraphy

Stratigraphy

Stratigraphy: the study of the 3-D spatial and temporal relationships among rocks

Page 4: Stratigraphy

Stratigraphy

• Principles of Stratigraphy

• Types of Stratigraphy

• Contacts

• Unconformities

Page 5: Stratigraphy

The oldest rocks are found on the bottom and the youngest rocks on the top.

youngest

oldest

Principles of Stratigraphy

1. Superposition

Page 6: Stratigraphy

youngest? oldest?

Principles of Stratigraphy

Page 7: Stratigraphy

older

younger

Principles of Stratigraphy

Page 8: Stratigraphy

sediments are deposited at the earth’s surface in flat layers

Principles of Stratigraphy

2. Original Horizontality

Page 9: Stratigraphy

Principles of Stratigraphy

Page 10: Stratigraphy

Principles of Stratigraphy

cross-bedding

Page 11: Stratigraphy

a bed will extend laterally until:

Principles of Stratigraphy

3. Lateral Continuity

1. Pinches out.

1. Abuts against older rock.

1. Truncated by erosion.

1. Cut by fault.

Page 12: Stratigraphy

Principles of Stratigraphy

Page 13: Stratigraphy

Rock that are cut by another geologic feature are older than the feature that cuts them.

Principles of Stratigraphy

4. Cross-Cutting Relationships

FaultErosion

IgneousIntrusion

Page 14: Stratigraphy

If pieces of rock A are included in rock B, rock A formed before rock B.

Principles of Stratigraphy

5. Rule of Inclusions

A

B

Page 15: Stratigraphy

6. Faunal Succession

Systematic sequence of fossils with time. Extinct fossils do not reappear in younger rocks.

Principles of Stratigraphy

http://www.geo.utexas.edu/courses/401/

Page 16: Stratigraphy

Stratigraphy

• Principles of Stratigraphy

• Types of Stratigraphy

• Contacts

• Unconformities

Page 17: Stratigraphy

Types of Stratigraphy

Lithostratigraphy Lithostratigraphic Unit Lithology

Pedostratigraphy Pedostratigraphic Unit Buried Soils

Biostratigraphy Bio Zones Fossil Content

Chronostratigraphy Chronostratigraphic Units

(Period, Epoch, Age)

Time Relationships

Geochronostratigraphy Geochronostratigraphic Unit

(System, Series, Stage)

Time Relationships

Magnetostratigraphy Magnetic Reversals, Chrons Magnetic Polarity

Chemostratigraphy Isotope Zones Chemical Characteristics

Sequence Stratigraphy Allostratigraphic Units unconformity-bounded packages

Type Subdivisions Property

Page 18: Stratigraphy

Types of Stratigraphy - Allostratigraphy

Page 19: Stratigraphy

Types of Stratigraphy

Lithostratigraphy Lithostratigraphic Unit Lithology

Pedostratigraphy Pedostratigraphic Unit Buried Soils

Biostratigraphy Bio Zones Fossil Content

Chronostratigraphy Chronostratigraphic Units

(Period, Epoch, Age)

Time Relationships

Geochronostratigraphy Geochronostratigraphic Unit

(System, Series, Stage)

Time Relationships

Magnetostratigraphy Magnetic Reversals, Chrons Magnetic Polarity

Chemostratigraphy Isotope Zones Chemical Characteristics

Sequence Stratigraphy Allostratigraphic Units unconformity-bounded packages

Type Subdivisions Property

Page 20: Stratigraphy

Types of Stratigraphy - Lithostratigraphy

Super Group

Group

*Formation

Member / Tongue / Lentil

Bed / Flow

*Formation: distinct, mappable rock body with definable boundaries

Page 21: Stratigraphy

Types of Stratigraphy

Lithostratigraphic Units

lens / lentil

(E. McBride)

Page 22: Stratigraphy

Stratigraphy

• Principles of Stratigraphy

• Types of Stratigraphy

• Contacts

• Unconformities

Page 23: Stratigraphy

Types of Contacts

• Intrusive

• Fault

• Depositional

- Conformable Contact

- Unconformity

Page 24: Stratigraphy

Types of Contacts (Depositional)

Ve

rtic

al C

on

tac

ts

Lateral Contacts

pinchout

intertonguing

gradation

inte

rca

late

dg

rad

ua

la

bru

pt

(Boggs, p. 453)

Page 25: Stratigraphy

Types of Contacts (Depositional)

Lateral Contacts

(E. McBride)

Page 26: Stratigraphy

Stratigraphy

• Principles of Stratigraphy

• Types of Stratigraphy

• Contacts

• Unconformities

Page 27: Stratigraphy

Unconformities

Unconformity: buried surface of erosion; missing rock / time

Hiatus: amount of missing time

Diastem: small amount of missing rock / time

vs

vs

Page 28: Stratigraphy

Uplift of Land

Erosion – Mechanical, Chemical, Biological

Drop in Sea Level

Unconformities

Page 29: Stratigraphy

Unconformities

Calvert Bluff / Alluvium Contact (Field Trip 1)

Page 30: Stratigraphy

Unconformities

Types:

• Disconformity

• Paraconformity

• Nonconformity

• Angular Unconformity

Page 31: Stratigraphy

• Disconformity – sediments on sediments (same orientation) with obvious erosion

Unconformities

Page 32: Stratigraphy

Redwall Limestone

Supai Group

Muav Limestone150 million years

20 million years

Disconformity

Unconformities

Page 33: Stratigraphy

Unconformities

2. Paraconformity – sediments on sediments (same orientation) no obvious erosion surface

(Boggs, p. 456)

Page 34: Stratigraphy

3. Angular unconformity – sediments on sediments (different orientations)

Unconformities

Page 35: Stratigraphy

250 million years

Angular Unconformity

Unconformities

Page 36: Stratigraphy

Angular Unconformity

Unconformities

Wyoming

Page 37: Stratigraphy

Angular Unconformity

Unconformities

(E. McBride)

Page 38: Stratigraphy

4. Nonconformity – sediments on crystalline igneous or metamorphic rocks

Unconformities

Erosional Surface

Uplift, Erosion, Deposition

Page 39: Stratigraphy

1800 million years

550 million years

Unconformities

Nonconformity

Page 40: Stratigraphy

Canadian Shield

Nonconformity in Progress

Enchanted Rock

Unconformities